Thursday, September 16, 2021

Rhodophyta (Red Algae): Definition, Characteristics, Reproduction, Examples and Role for Life

Rhodophyta (Red algae)"Rhodophyta (Red algae)" by Ed Bierman is licensed under CC BY 2.0

 Definition of Rhodophyta (Red Algae)

The term "Rhodophyta" comes from the Greek,  rhodos  which means "red". So, Rhodophyta means red algae ( red algae ). Unlike other phyla, this phylum does not have flagella stages in its life cycle. Members of this phylum have photosynthetic pigments in the form of phycobilins consisting of  phycoerythrin  (red pigment) and  phycocyanin  (blue pigment). In addition to these two pigments, Rhodophyta also has chlorophyll a and b and carotenoids.

Phycoerythrin is the most dominant pigment that causes the color of the thallus of this algae to turn red. However, not all of these algae are red. In the deep sea, this algae has a purple almost black color. At medium depths it is bright red, while at very shallow water, it is slightly greenish.

When this has been known for about 2,500 species, mostly live in the sea, especially the tropics and often called  kelp  ( sea weed ) because of her body shape like grass. Rhodophyta grows on rocks in tidal areas to depths of up to 90 meters below sea level where certain light waves from sunlight are still able to reach them.

Rhodophyta thallus is relatively large, but rarely exceeds 90 cm in length. Some species are filamentous, but most form complex structures that branch like feathers or are flattened and spread like ribbons. Generally, Rhodophyta are multicellular, but there are also unicellular Rhodophytes. Multicellular red algae are generally macroscopic and their body structure resembles a plant ( thallus ). Thallus in Rhodophyta in the form of strands or like plants.

Characteristics of Rhodophyta (Red Algae)

Red algae (Rhodophyta) have general characteristics or characteristics, including the following.

■ Core are eukaryotic cells because the cell nucleus already had membranes.  

■ Most multicellular (multicellular).  

■ Generally, macroscopic (visible with the naked eye) with a length of 1 m.  

■ The only algae that do not have flagella phase in its life cycle.  

■ Characteristically autotorof, because chlorophyll to perform photosynthesis.  

■ The chloroplasts contain pirenoid to store the results of photosynthesis.  

■ Backup food is stored in the form of flour fluoride (a type of carbohydrate), floridosid (compounds of glycerine and galactose) and drops of oil. Floridoside will have a reddish color when added with iodine.  

■ The shape of the talus in the form of a strand or shaped like a tree.  

The thallus is red to purple in color but some are blonde or reddish.  

■ His body was covered with calcium carbonate (CaCO 3 ).  

■ The cell walls consist of layered components. The inner cell wall is composed of myofibrils, while the outer cell is composed of mucus.  

■ Have pigment chlorophyll a and b, carotenoids, phycocyanin (blue) and the dominant pigment fikoeritrin (red).  

How to Reproduction Rhodophyta (Red Algae)

Red algae can reproduce asexually (vegetatively) and sexually (generatively). Asexual reproduction by forming aplanospores , namely nonmotile spores (not moving) and derived from diploid algae thallus. Furthermore, these spores will grow into new red algae. In Rhodophyta, fragmentation asexual reproduction is rare.

Sexual reproduction (generative) occurs by  oogamy , and in some species undergo alternation of offspring (metagenesis). Sexual reproduction is carried out by the fusion of male gametes that have no locomotion (sperm) and ova. The male gametes are formed in the spermatangium, while the female gametes are formed in the carpogonium. The next fertilized zygote will grow into a diploid red algae.

The following is a life cycle chart or alternation of offspring in an example of a red algae species, Polysiphonia.

Based on the picture above, try to write down the sequence of asexual (vegetative) reproduction starting from the sporophyte. Then, also write down the sequence of sexual reproduction (generative) to the sporophyte!

The sporophyte produces  meiospores  which will develop into gametophytes. The gametophyte forms  spermatangia  which produce  spermatia  and carpogonium  which contains  trichogen cells . The spermatia attach to the tip of the trichogen, continuing to enter the base of the cell. Here the fusion occurs between the nucleus of the sperm and the nucleus of the female cell to form a zygote (goninoblast).  Goninoblast  is a filament that is formed from the zygote and at the end of the filament a carposporangium is formed .

Furthermore, in the carposporangium formed carpospora.  Carpospora  out of the carposporangium, to further grow into a sporophyte (new Polysphonia). In its growth, Polysiphonia undergo alternation of offspring (metagenesis), namely asexual reproduction and sexual reproduction take place alternately.

Examples and Roles of Rhodophyta (Red Algae) in Life

Some red algae serve as important supports for tropical coral reefs. Red algae is an important food ingredient in Asian countries. In Japan, for example, red algae are dried and used in a number of dishes. In addition to producing algin, red algae also produce carrageenan and agar.

Carrageenan ( carrageenan ) is a type of polysaccharide used as an ingredient in cosmetics and gelatin capsules and is an additive that can be added to puddings and ice cream. To be used as food. Apart from being used as a food ingredient, agar-agar is also used as a medium for microorganism culture, cosmetics, medicine, canned meat coating, ice cream hardener, as well as fat emulsifier and chocolate bars.

Some examples of Rodophyta are as follows.

■ Eucheuma spinosum , widely cultivated because it produces so many are in Indonesian waters.  

■ Chondrus crispus , also cultivated known as seaweed.  

■ Gelidium coulteri  and  Gracilaria sp. , as an ingredient for making gelatin, is widely available in cold waters of the country.  

■ Carolina sp.  is a member of Rhodophyta (red algae) whose body is coated by calcium carbonate.  

■ Dasya, Batracnospermum, Scinaiafurcellata,  Porphyra perforated , Polysphonia,  Halosaccion glandiforme ,  Bossea orbigniana , and so on.

Phaeophyta (Brown Algae): Definition, Characteristics, Classification, Reproduction, Examples and Role for Life

Phaeophyta Fucus receptacle 03"Phaeophyta Fucus receptacle 03" by Bruce Kirchoff is licensed under CC BY 2.0

 Definition of Phaeophyta (Brown Algae)

Brown algae are plant-like protists that have many-celled thallus, so they can be seen macroscopically (with the naked eye). The thallus has an adhesive device to attach its body to the substrate, while the rest of the body floats on the water. Some members of the Phylum Phaeophyta such as Sargassum, Macrocystis, and Nereocystis have air bubbles that function to store nitrogen gas and to float on the surface of the water.

Brown algae contain brown pigments (xanthophylls), chlorophyll a and c. The amount of xanthophyll pigment is dominant, causing the color of the thallus to be brown. Food reserves are stored in the form of laminarin. Generally, brown algae are multicellular (multicellular). Its body shape resembles higher plants because it has parts resembling roots, stems, and leaves, making this algae easy to identify.

About 1,500 species of Phaeophyta or brown algae are known. Almost all types of Phaeophyta live in the sea, especially in cold areas, which live on rocks at the bottom of the water as deep as 1.5  -  5 meters from the water surface. All brown algae are threads or sheets and are autotrophic (capable of producing their own food).

All Phaeophyta live in colonies with shapes varying from simple to large ones with complex cell organization. In large colonies of Phaeophyta, no real organs have yet been formed, although in some species there are shapes resembling roots, stems, and leaves, the whole part is referred to as a thallus.

Characteristics of Phaeophyta (Brown Algae)

Brown algae (Phaeophyta) have general characteristics or characteristics, which are as follows.

■ Core are eukaryotic cells because the cell nucleus already had membranes.  

■ multicellular (multicellular).  

■ Shaped sheet, and some even resembling a tall plant (Plantae) because it has a section resembling roots, stems, and leaves.  

■ It has air bubbles that served as a float.  

■ Had the talus microscopic to macroscopic size.  

■ Have pigment chlorophyll a, chlorophyll c, violaxantin, b-carotene, diadinoxantin, as well as the amount xantofil dominant.  

In the form of branched filaments, unbranched and some are erect.  

■ Characteristically autotorof, because chlorophyll to perform photosynthesis.  

■ Having a single chloroplast some thread-like disk-shaped (discoid).  

■ The chloroplasts contain pirenois to store food reserves.  

■ Backup stored food in the form of laminarin.  

■ Have a cell wall.  

■ In the cell wall and intercellular space are agen (alginate acid), the inside of the cell wall composed of cellulose layers.  

■ Having a network of transportation such as higher plants.  

■ Almost all types of Phaeophyta habitat in the ocean, especially in the cold, that live in the rocks in the bottom waters as deep as 1,5  -  5 meters from the water's surface.  

■ All Phaeophyta live in colonies with varied shapes from the simple to the form of large (over 30 meters) with complex cellular organization.

Classification of Phaeophyta (Brown Algae)

■ Laminaria , has a stem, the leaf-shaped sheets, containing iodine and alginic acid.  

■ Macrocystis , produces iodine and alginic acid that serves as an industrial material.  

■ Sargasum , sheet-shaped leaves, between the stem and the stem there are air bubbles.  

■ Fucus , leaf shape in the form of sheets and at the edges of the leaves are bubbles.

Methods of Reproduction of Phaeophyta (Brown Algae)

Reproduction in Phaeophyta is done asexually (vegetatively) and sexually (generatively). Brown algae asexual reproduction is done by fragmentation  and  formation of spores  (aplanospores and zoospores). The resulting zoospores have flagella that are unequal in length and are located on the lateral side (sides or edges).

Meanwhile, sexual reproduction is done by  isogamy ,  anisogamy , or  oogamy . Fucus vesiculosis is an example of brown algae that reproduces oogamously. There is a way of generative/sexual reproduction of brown algae which is similar to higher plants, namely the ends of the fertile thallus sheets form a body containing reproductive organs called  receptacles .

Inside this receptacle there is a  conceptacle  containing antheridia which produces male sex cells in the form of spermatozoa and oogonia which produce eggs (ova) and sterile threads called paraphysis. The antheridia are funnel-shaped cells that arise from the base and edges of the conceptacle, the oogonia are bodies that sit on top of the stalk.

If a spermatozoon can fertilize an egg, a zygote will be formed. The zygote then forms a thick wall of cellulose and pectin, then attaches to a substrate such as rocks, then grows into a new individual whose chromosomes are diploid.

Examples and Roles of Phaeophyta (Brown Algae) in Life

Many types of Phaeophyta are beneficial to humans. Some species produce human food. In other countries kelp is used for animal feed and fertilizer, because the nitrogen and potassium content is high but the phosphorus content is low. Phaeophyta also produce algin (alginic acid), a colloid that is useful as a stabilizer in the manufacture of ice cream. Algin is also important in the pharmaceutical industry, namely as an ingredient for making pills, tablets, ointments, and dental cleaning drugs.

Some examples of Phaeophyta are as follows.

■ Fucus vesiculosus , height can reach 30  -  100 cm, live attached to rocks that appear when water is low. There are air bubbles along the sides of the thallus that branch like a fork. The tip is enlarged to form a conceptacle.  

■ Sargassum siliquosum , live attached to rocks along the rocky coast of the tropics. However, on the northern Atlantic coast, the species of  Sargasssum natans  floats freely on the sea surface. Sargassum sizes vary from small to hundreds of meters in length.  

■ Macrocystis integrifolia  or  kelp , size is very large, on the west coast of North America are found in length can reach three kilometers. Living kelp is firmly attached to rocks with the help of a root-like thallus.  

■ Laminaria sinclairii  is a type of brown algae producer alginic acid needed for the production of textiles, food, and cosmetics.  

■ Fucus serratus , including brown algae that differentiate into a form that floats.  

■ Postelsia  is an example that many common brown algae.  

■ Turbinaria decurens ,  Dictyota sp .,  Dictyosiphon sp .,  Nereocystis sp . is another example of Phaeophyta species or brown algae.


Chlorophyta (Green Algae): Definition, Characteristics, Classification, Reproduction, Examples and Role for Life

Green Feather Algae (Caulerpa sertularioides)"Green Feather Algae (Caulerpa sertularioides)" by bob in swamp is licensed under CC BY 2.0

 Definition of Chlorophyta (Green Algae)

Green algae ( green algae ) are named based on the chloroplast are colored green. This green color exists because the dominant pigments are chlorophyll a  and  chlorophyll  b , in addition to other types of pigments, namely carotene and xanthophyll. The shape of the chloroplast in green algae varies, some are bowl-like (for example in  Chlamidomonas ), spiral (for example in  Spirogyra ), and shaped like stars.

Although green algae are called algae, they are structurally and biochemically closer to plants. Today even many botanists (plant experts) who include it in the group of plants. Like plants, green algae store carbohydrates in the form of starch grains in their chloroplasts. The cell walls of some species of Chlorophyta are made up of cellulose, pectin, and other polysaccharides, such as plant cell walls.

Green algae are plankton that live floating in fresh water or sea. In addition to fresh water or sea, green algae also have a habitat in wet soils and some in dry places. Because it has chlorophyll, these algae can carry out photosynthesis and are autotrophs (can make their own food).

With the help of sunlight, Chlorophyta can carry out photosynthesis. Plankton is the main food source for animals that live in water. Plankton are referred to as producers. How do you know if Chlorophyta is doing photosynthesis?

Observe and pay attention to freshwater fish ponds during the day. If you pay close attention, algae exposed to sunlight will release gas in the form of small bubbles that stick to the edges of the pool, the gas is oxygen. Oxygen is a gas produced in the process of photosynthesis.

Chlorophyta or green algae consist of  ±  7,000 species that live in waters and on land. Some green algae live in seawater, but most live in fresh water. There are green algae that live solitary and some are colonies. Unicellular green algae can move freely because they have flagella. Some types of green algae that colonize have attachments to the substrate that help them to stick firmly to the rocks at the bottom of the water.

Characteristics of Chlorophyta (Green Algae)

Green algae (Chlorophyta) have the following characteristics or general characteristics.

The body contains chlorophyll and is green in color. Cells contain chloroplasts which contain chlorophyll a, chlorophyll b, carotene and xanthophylls.  

■ Core are eukaryotic cells because the cell nucleus already had membranes.  

■ Has had a cell wall composed of cellulose.  

■ Life floated in fresh water or sea water and acts as plankton as a food source of aquatic organisms.  

■ There are unicellular (single-celled) and some are multicellular (multicellular) simple.  

■ Characteristically autotorof, because chlorophyll to perform photosynthesis.  

■ There is a solitary life (his own), colonize (groups) and there is also a form of symbiosis with other organisms. One example of a well-known mutualism symbiosis is the symbiosis between Chlorophyta and Fungi (fungi) forming  Lichenes  (lichens).  

■ Body shape varies, some round, shaped filamentous (thread form), there is nothing like the sheets and higher plants.  

■ The shape of chloroplasts assortment, there is nothing like Mangkung, spiral, star, mesh, and some are like sponges.  

■ Have pirenoid as a storage area of photosynthesis in the form of starch and fat.  

■ In addition to chloroplasts, the organelles that owned Chlorophyta include the Golgi apparatus, mitochondria and endoplasmic reticulum (ER).  

■ Have a stigma (red eye spots) for green algae are motile (moving). This stigma serves to guide the algae towards light so that photosynthesis can occur.  

■ Have one or two flagella are the same size for the length of motile green algae.  

■ Have a contractile vacuole as osmoregulasi tool to regulate the osmotic pressure.  

■ Having a permanent body shape.  

■ Have habitats in freshwater, marine, wet soils, but some are in a dry place. 90% of Chlorophyta live in fresh water and 10% live in the sea as plankton or benthos, in the soil and attached to other organisms.

Classification of Chlorophyta (Green Algae)

Based on the shape and whether or not they can move, green algae are divided into 6 genera, namely:

■ Algae / celled green algae is not moving  

Example:

1)  Chlorella sp.  spherical in shape, live in fresh water or sea water, reproduce vegetatively by dividing, widely used to study photosynthesis.

2)  Cholococcum sp.  spherical in shape, live in fresh water, reproduce vegetatively by forming zoospores generatively with isogamy.

■ Algae / celled green algae can move  

Example:

1)  Chlamydomonas sp.  ovoid, has two flagella, chloroplasts are cup-shaped or ribbon-shaped containing pyrenoids and stigma. Reproduction by division and conjugation

2)  Euglena viridis , shaped like an eye, has a flagellum, chlorophyll and sigma. Reproduction by dividing. Euglena there also group it into Protozoa .

■ algae / green algae form colonies do not move  

Example:  Hydrodictyon sp. , the colonies are net-shaped, mostly found in fresh water, reproduce vegetatively by fragmentation and generatively by conjugation.

■ algae / green algae shaped colonies that move  

Example:  Volvox globator , the shape of the colony resembles a ball composed of thousands of volvox which are connected to each other by cytoplasmic threads. Volvox is also grouped into Protozoa.

■ algae / green algae form filaments (yarn)  

Example:

1)  Spirogyra sp.  (unbranched thread, single nucleus, spirally arranged ribbon-shaped chloroplast, many pyrenoids).

2)  Oedogonium sp.  (unbranched filaments, mesh-shaped chloroplasts, many pyrenoids, one large nucleus).

■ Algae / thalus shaped green algae (sheet)  

Example:

1)  Ulva lactua  (sea lettuce), the shape of a sheet like a leaf and lives in the sea attached to a rock, can be eaten. Reproduction vegetatively by forming zoospores and sexually by isogamy.

1)  Chara sp. , shaped like a tall plant, has stems and branches that are segmented, live in fresh water. Reproduction vegetatively by fragmentation and generatively by the meeting of egg cells produced by the oogonia and sperm cells produced by the antheridium.

How to Reproduction Chlorophyta (Green Algae)

This green algae can reproduce asexually (vegetatively) and also sexually (generatively).

Reproduction Asexually (Vegetatively)

■ Establishment of  zoospores  (spores wanderer). These spores have 4 hairs, contractile vacuoles, most have 1 eye spot (stigma), and can move by swimming because they have flagella.  

■ binary fission. Green algae that reproduce by binary fission, usually carried out by single-celled algae (unicellular).  

■ Fragmentation. Green algae that reproduce by fragmentation by thread-shaped algae or those in colonies.  

Sexual Reproduction (Generative)

■ anisogamy. Recall what happened to Cyanophyta . In addition to asexually, green algae can also reproduce sexually (generatively), namely by  anisogamy . The male gamete is always free-moving which closely resembles a zoospore, while the female gamete is sometimes immobile, so it is an oogonia. After mating, it will produce a zygote which will then grow into a new algae.  

■ Conjugation. In addition, there are also green algae whose sexual reproduction takes place by conjugation, namely the fusion of two gametes to form a zygospore. This zygospore has no locomotion, so it cannot move.

Examples and Roles of Chlorophyta (Green Algae) in Life

Some examples of types of green algae include Chlamydomonas, Volvox, Protococcus, Spyrogyra, Ulothrix, Oedogonium, Chlorella, Chlorococcum, Ulva, and Chara. The following is an explanation of the characteristics, body structure and reproduction methods of several types of green algae and their benefits in life (if any).

Chlorococcum and Chlorella are single-celled Chlorophyta that cannot move and are microscopic. The chloroplasts are bowl-shaped, microscopic in size, and live as freshwater plankton. Chlorococcum and Chlorella can reproduce asexually by forming zoospores that move with two flagella. Chlorella can reproduce by cell division.

Chlorella can be used as a drug, even now being developed for drugs that are packaged in capsule form. Chlorella also gives great hope to overcome the need for alternative food ingredients in the future. Reproduction is very fast in a good environment, the ideal temperature for photosynthesis is around 25 o  C.

The process in the Chlorella laboratory is used in photosynthesis research. In photosynthesis it produces carbohydrates, proteins and fats. Organic substances, carbon dioxide and minerals are applied to the substrate and the light intensity and duration of irradiation can be adjusted to produce the desired carbohydrates, fats and proteins.

Chlamydomonas is a single-celled Chlorophyta that can move and is microscopic. The cells are ovoid in shape. Chlamydomonas cells contain one nucleus, one vacuole, and chloroplasts. The locomotion consists of two flagella. Cup shaped chloroplasts. Eyespots and pyrenoids are located in the bowl which serves as a place for the formation of starch. Chlamydomonas can reproduce in two ways, namely by the formation of zoospores and conjugation.

Spirogyra and Oedogonium are cells that form threads or elongated strands like threads and are microscopic. Spirogyra and Oedogonium mostly live in fresh water. Spirogyra have cells containing chloroplasts in the form of spiral bands and in one cell containing one nucleus, can reproduce by fragmentation and conjugation.

Oedogonium has mesh-shaped chloroplasts and in one cell contains one nucleus and can reproduce by zoospores and the fusion of spermatozoa (antheridium) with ova (oogonia) produced by different threads. The result of the fusion is a zygote that can grow into a new individual.

Chara and Ulva are Chlorophyta in sheet form. Chara is an algae that lives in fresh water, has segments that contain nucules and globules. The nucleus contains the ovum-producing archegonia. The globules contain spermatozoid-producing antheridia. Fertilization of an ovum by a spermatozoon will produce a zygospore which will then develop into a new individual. Asexual reproduction is done by fragmentation.

The ulva has a thallus in the form of a sheet consisting of two layers of cells. The shape of the Ulva thallus is like a lettuce leaf, the chloroplast is cup-shaped. Ulva can live in brackish water, salt water, or attached to wood and rocks along the coast. Ulva reproduces asexually with zoospores with fla agella and will form haploid Ulva. Sexual reproduction is characterized by the union of male and female sex cells to form a zygote. The zygote will develop into a diploid Ulva.

Hydrodictyon is a Chlorophyta in the form of immobile colonies. It is found in fresh water and forms a net-like colony. Reproduce asexually by spores and fragmentation, while sexually by conjugation.

Volvox is a Chlorophyta that is in the form of colonies and moves. Volvox live in fresh water and each cell has two flagella and stigma, a spherical colony with a cell number of 500 –  50,000 cells  . Asexual reproduction is done by fragmentation, while sexually by conjugation.


Wednesday, September 15, 2021

Definition of Protozoa and Their Characteristics, Classification and Production

Protozoa"Protozoa" by Louisiana Sea Grant is licensed under CC BY 2.0

 Definition of Protozoa

Protozoa is one of the groups (sub kingdom) of members of the protists of eukaryotes. Protozoa comes from the Greek, namely protos means first and zoon  means animal. So, protozoa are the first animals or simply low-level animals that only have one cell. Protozoa habitat is in watery places that are rich in organic substances for example Amoeba proteus , both fresh and salt water, some live solitaire free to swim in water, stick to one place, parasite on plants and animals as well as humans as symbionts and are detrimental because as a cause disease is even beneficial because it helps destroy or decompose dead organisms.

Protozoa are single-celled animals, true nuclei (eukaryotic) and do not have a cell wall. Protozoa comes from the word protos which means first and zoon  which means animal so it is called the first animal. The size is between 3 - 1000 microns and is a microscopic organism that is heterotrophic.

The morphology of protozoa varies, their physiology and metabolism adapted to their needs; nutrients are heterotrophic in free-living parasitic and autotrophic forms, they have a more or less complex life cycle, both free-living and parasitic, and in most cases, vegetative forms (trophozoites) and other resistant forms (cysts).

Protozoa are very diverse in shape and size. Some are oval or spherical, some are elongated, some are polymorphic (having various morphological forms at different stages in their life cycle). Some protozoa are as small as 1 nanometer in diameter; others, such as Amoeba proteus measuring 600 nanometers or more. Some common ciliates reach a size of 2,000 nanometers or 2 mm, so they can be seen easily without magnification.

General Characteristics of Protozoa

Protozoa are eukaryotic (nucleus protected by nuclear membrane) so that genetic substance / chromosomes are separated from the cytoplasm because there is a nuclear membrane barrier (caryotheca).

Cell does not have a cell wall, but if the environment is less well able to form a thick protective layer called cysts or cystic after good environment cyst rupture.

Cell shape is generally fixed except for Rhizopods.

Heterotrophs means that their food depends on other organisms (foraging for food by phagocytosis or pinocytosis).

In the food chain as zooplankton.

Some species are parasitic and cause disease in humans and livestock.

Has a different body shape at each phase in its life cycle.

Some protozoa have an active vegetative phase called trophozoites and a dormant phase in the form of cysts . Trophozoites will actively forage and produce as long as environmental conditions permit. If conditions do not allow the life of trophozoites, the protozoa will form cysts .

Cysta is a form of protozoan cells that are dehydrated and thick-walled similar to the endospores that occur in bacteria. At the time of the protozoan cysts are able to survive in a dry or wet environment.

Generally reproduce by dividing, there is also a conjugation.

Protozoa have locomotion tools that are in the form of pseudo-legs, vibrating hairs (cillia) and whip feathers (flagels) or with the cells themselves.

Nutrient uptake is by holozoic (eating other living organisms), saprozoic (eating dead organisms), holophytic or autotrophs (can form their own food through photosynthesis), saprozoic (absorbing dissolved substances around them).

How Protozoa Find Food

Protozoa are inhabitants of wet and watery places that are rich in organic substances, such as ditches, rice fields, ditches, rivers, reservoirs, seas, or parasites live in the bodies of other organisms. In places that are waterlogged and contain dry grass, protozoa are also often found. At the unfavorable environment, protozoan cysts can wrap yourself as a material composed of calcium carbonate (CaCO 3 ).

protozoa in taking food are carried out in the following ways:

Holozoic , which takes food from other microorganisms such as bacteria or algae (algae).

Saprophyte , which takes food from the crushed plant material around it.

Saprozoic , which takes food from animals that have died.

Holozoic , that is by carrying out photosynthesis

Classification and Examples of Protozoa

Based on the locomotion they have, the protozoa are divided into four classes, namely rhizopoda, mastigophora, sporozoa and ciliates.

Rhizopoda or Sarcodina

Rhizopoda or Sarcodina (Rhizoid = root, podos = foot) are protozoa that move using pseudopodia (false feet) which are extensions of the cytoplasm, for example Amoeba , Foraminifera, Radiolaria, Arcella, Entamoeba coli, and Entamoeba histolytica . Is a microscopic animal that lives as a small mass that is clear and amorphous or can change its shape.

The rhizopoda class is divided into 5 orders, namely:

1. Order Lobosa, characterized by short and blunt pseudopodia and clear differences between ectoplasm and endoplasm.

2. Order philose, characteristics: have pseudopodia smooth like threads and branches.

3. Order foraminifera, characteristics: have long and smooth pseudopodia.

4. The order helioza, characterized by: has pseudopodia in the form of radial threads and the interfilaments never unite to form a net or webbing.

5. Order radiolarian, characterized: have pseudopodia in the form of fine threads arranged radially and branched to form a net (woven).

The body structure contains the nucleus, food vacuola, cytoplasm and others. For free-living animals there are contractile vacuoles (contractile vacuoles are found in all freshwater rhizopods), while parasitic animals are absent. Contractile vacuole functions as an osmoregulator or water balance regulator but can also function as a means of excretion.

Some species have a graft or shell to protect the cell. The shell is made of silicon (eg Radiolaria) or calcium carbonate (eg Foraminifera). Both live in the sea. If the animal dies, the shell remains intact for a long time so that it can turn into fossils. Fossils This is used to determine the age of the earth's layers or as an indication of the history of the earth. Besides that, another function is used as an indication of the presence of petroleum sources. The behavior of rhizopods is based on stimuli or responses to various external and internal stimuli due to the sensitivity of their protoplasm. This is because they do not have a nervous system. . Members of the class rhizopoda reproduce by binary fission and digestion of food is carried out internally in food vacuoles.While respiration is done by diffusion.

Examples of members of the rhizopoda class and their benefits or disadvantages:

1. Entamoeba histolytica, causes amoebic dysentery (as opposed to bacillary dysentery caused by Shigella dysentriae)

2. Entamoeba gingivalis, causes food spoilage in the mouth resulting in inflammation of the gums (Gingivitis)

3. Entamoeba coli, helps the formation of vitamin K

4. Foraminifera sp, its fossils can be used as an indication of the presence of petroleum. Soils containing fossils of Foraminifera are called globigerina soils.

5. Radiolaria sp, soil sediment containing the animal is used as a scouring agent.

6. Entamoeba coli that lives in the intestines of cows can help the digestion of cows.

Mastigophora or Flagellates

Flagellata comes from the word flagellum which means whip feathers. Thus, organisms belonging to the phylum Flagellata all have whip feathers. phylum flagellata also called mastigophora ( mastix : whip feathers and phoros : carry). Flagella or whip feathers, apart from being a means of locomotion, also function as a tool for touching and catching food.

Flagella also function as sensory organs. The flagellates are a unique group of protozoa. Some of its members have chlorophyll so some group it into algae. Based on the presence or absence of chlorophyll, flagellates are divided into phytoflagellates and zooflagellates.

Has a body wall in the form of a pellicle, so the shape is relatively fixed with a size of approximately 0.1 mm. Has a nucleus and in some species has chloroplasts with chlorophyll that functions for photosynthesis, which are included in the phytonagellate group.

Free-living members of the mastigophora class have contractile vacuoles, while parasitic animals do not. Respiration and excretion are carried out by diffusion by the body surface.

How to reproduce mastigophores, namely:

Vegetative: binary fission, longitudinally. For example Euglena viridis

Generative: occurs in flagellates that colonize, for example Volvox sp.

Sperm x Ovum →Fertilization →Zygote → Zygospore → Zoospore → New individual

Digestion is carried out by flagellar movement causing a flow that pushes food towards the cells to be swallowed through the mouth. Then it goes to the cytopharynx and is digested in the food vacuole. In flagellate saprophytic nutrition (live by destroying objects around it) digestion is carried out by absorption.

The parasitic mastighopora are the genus Trypanosoma and the genus Trichomonas.

1. Trypanosoma gambiense and Trypanosoma rhodesiense, are parasites in human blood plasma and can cause sleeping sickness. In Africa, transmission is carried out by the Tse-tse fly, namely Glosina palpalis.

2. Trypanasoma cruzi, Chagas disease in America

3. Trypanosoma evansi, sura disease in animals

4. Trypanosoma brucei, Nagana disease in cattle and buffalo

5. Trypansoma vaginalis, the cause of vaginal discharge in women

6. Trypanosoma foetus, a parasite in cow's vagina

Sporozoa (Apicomplexa)

Sporozoa has a simple elliptical body with a nucleus. It has no locomotion or (moves with the cell itself) or contractile vacuole. It is called Sporozoa because at certain stages in its life, it can form a kind of spore.

Almost all members of the sporozoa are parasites, so that food is taken directly from the host. Has a nucleus and at the time of double division, the nucleus divides repeatedly, each nucleus forms a wrapper and finally produces quite a lot of individual offspring. The sporozoa carry out respiration and excretion by diffusion.

Vegetative (asexual) reproduction is also called Schizogony and generative (sexual) is called Sporogony. Vegetatively, namely through multiple divisions so that many individual children are produced. On a generative way, namely through alternation of offspring between the vegetative phase in the human body and the generative phase in the body of an intermediate host such as Plasmodium with a generative phase in female Anopheles  mosquitoes .

The reproduction or life cycle can be divided into three stages:

  • Schizogoni, formed by dividing and occurs after infecting the host
  • Sporogony, the formation of spores outside the host and is an effective stage.
  • Gamogony / gametogenesis, the stage of formation of gamete cells occurs in the body of an intermediate host or mosquito.

Ciliates (Ciliophora/Infusoria)

Has a relatively fixed shape and moves with vibrating hair or called cilia. Has a nucleus and some species have more than one nucleus, for example Paramecium a urelia . Live in watery places, for example: rice fields, swamps, watery soil and contain lots of organic matter. For free-living there are contractile vacuoles, while parasitic animals do not exist. Respiration and excretion through the body surface.

Digestion of food internally in the food vacuole. While the way to catch food is by vibrating the hair (cilia), then there is a flow of water out and into the mouth of the cell. That's when water enters bacteria, organic matter or other unicellular animals.

There are free-living members of the ciliates such as Paramecium candatum and those that live as parasites such as Nyctoterus ovalis  and Balantidium coli.

Ciliates reproduce by:

1. Asexual

Asexual or by dividing themselves by binary fission where the cell divides into 2 then into 4, 8 and 16 and so on. Cleavage begins with division of the micronucleus and is followed by division of the macronucleus.

2. Sexual (conjugation)

The trick is that the two cells approach each other, sticking to the mouth of the cell to mate. This means that these two animals are undergoing conjugation. Furthermore, a conjugation channel is formed between these two cells. And through this channel the micronucleus exchange occurs. The micronucleus from one cell moves to another cell, and vice versa. 

While other examples of Ciliata animals are 

a. Stentor, living in rice fields or stagnant water contains a lot of organic matter. 

b. Didinium, a predator of Paramecium, lives in waters that are abundant in protozoa. 

c. Vorticella, shaped like a bell, cilia are scattered around the mouth of the cell. 

d. Stylonichia, similar to Paramecium, cilia in groups called cirrus, live in waters that contain lots of organic waste.

Benefits of Ecosystem Protozoa

Protozoa and algae are also contributors to soil biomass in lowland rice cultivation. Another important role of protozoa and algae is as a bioindicator of environmental change.

Protozoa that live in fresh water and sea water are zooplankton which are food for aquatic insects, shrimp, and small fish. Zooplankton is a source of food for aquatic animals, including fish. So that the protozoa benefit humans. Because fish eat protozoa and humans eat fish.

Entamoeba coli that lives in the intestines of cows is beneficial, because it can help the digestion of cattle. Thus there is a symbiotic mutualism between the ox and Entamoeba. Cows are helped to digest grasses that contain tough cellulose, while Entamoeba gets food and protection.

The benefits of protozoa for humans

Most of the zooplankton in aquatic ecosystems are chlorophyll protists that are useful as food for fish and aquatic arthropods.

Ent amoeba coli in the large intestine of mammals plays a role in the process of decaying food waste.

Foraminifera have an exoskeleton of limestone and fossils in a certain amount can form globigerina soil deposits which can be used as an indication of the presence of petroleum.

Radiolaria have a skeleton made of grit. The dead radiolarians will leave their shells and form radiolarian soil that can be used as an abrasive.

Paramecium can also be used as an indicator organism of water pollution by organic substances.

Chlorella besides acting as a producer in aquatic ecosystems, it can also be used as a basic ingredient for making single cell proteins.

Monday, September 13, 2021

Metamorphic Rocks: Definition, Types and Impacts

Gneiss 1"Gneiss 1" by James St. John is licensed under CC BY 2.0

 Definition of Metamorphic Rock

There are many types of rock. One type of rock is metamorphic rock. This metamorphic name is a name for the type of rock that complements igneous and sedimentary rocks. This metamorphic rock is often referred to as metamorphic rock. Metamorphic rock or metamorphic rock is a group of rocks that are the result of the alteration or transformation of a pre-existing rock type (protolith) by a process called metamorphosis or changing shape.

This metamorphic rock has very important uses for humans. Through research conducted on these metamorphic rocks can be obtained very important information about the temperature and pressure that occurs deep in the earth's surface. However, nowadays many metamorphic rocks have been exposed on the earth's surface due to soil erosion and uplift.

The Process of Occurrence of Metamorphic Rocks

This metamorphic rock is not a type of rock that directly exists in this world. To turn into metamorphic rock, it takes several processes. The process of the occurrence of these metamorphic rocks comes from pre-existing rocks, namely protoliths. Protolith or original rock that is subjected to heat of more than 150 degrees Celsius and also extreme pressure will experience major physical or chemical changes. There are many types of protolith rocks. Included in this protolith rock are igneous rock, sedimentary rock, or it could be other metamorphic rocks of older age such as Gneiss, slate, marble, and schist stones.

Types of Metamorphic Rocks

 There are various types of Metamorphic Rocks and not just one. This metamorphic rock can be divided into three types, namely contact metamorphic rock, dynamo metamorphic odor, and pneumatolist contact metamorphic rock. To get to know each of these metamorphic rocks closer, we will discuss them one by one.

Contact metamorphic rock

The first type of metamorphic rock we will discuss is the contact metamorphic rock type. Contact metamorphic rock is a type of metamorphic rock that undergoes metamorphosis as a result of very high temperatures or as a result of magma activity. There are also those who state that these contact metamorphic rocks are rocks formed due to the influence of magma intrusion at very high temperatures. The existence of very high temperatures originating from this magma activity causes changes in the shape and color of the rock. This high temperature is also due to its proximity to magma. Examples of these contact metamorphic rocks are limestone or limestone into marble, then batholiths, lacolitic rocks, and sill rocks. One thing we need to know about this type of rock,that is, this type of rock is influenced by the location of the intrusion, where the farther it is from the intrusion, the degree of metamorphosis will decrease.

Dynamo metamorphic rock

The second type of metamorphic rock is dynamo metamorphic rock. Dynamo metamorphic rock is a type of rock that undergoes metamorphosis as a result of high pressure originating from endogenous forces for a long time, and is produced in the process of forming the earth's crust due to endogenous forces. This dynamo metamorphic rock usually occurs or is in the upper part of the earth's crust. The existence of pressure in the opposite direction causes changes in mineral grains, some are flat and some are back into crystal form. Some of these types of metamorphic rocks turn into crystals. Examples are pulverized rock and shale. Another example of dynamo metamorphic rock is mud stone or mud stone into slate or slate. This type of rock is often found in areas of faults or folds.

Pneumatolytic contact metamorphic rocks

The next type of metamorphic rock is pneumatolist contact metamorphic rock. This type of rock is a rock that undergoes a metamorphic process as a result of the influence of the gases present in the magma. The influence of this hot gas causes changes in the chemical composition of the minerals of this rock. An example of a pneumatolist contact metamorphic rock is quartz with borium gas turning into tourmaline or a kind of gemstone. Another example of this type of stone is quartz stone with fluorium gas and housed into topaz.

Those are the kinds or types of metamorphic rocks that are around us or that we often encounter. Metamorphic rock is basically a type of rock that has undergone a metamorphic process. Metamorphosis that occurs in rock itself is a process in which an object changes form from one form to another. In this stone metamorphosis, the metamorphosis process consists of various kinds and not just one.

Types of Metamorphic Rock Metamorphic

Metamorphic rock is a type of rock that undergoes a metamorphic or metamorphic process. The process of rock metamorphism itself consists of three kinds, namely thermal metamorphosis, dynamo metamorphosis, and also regional metamorphosis. Then, what exactly is the meaning of each type of metamorphosis?

Thermal Metamorphosis

Thermal metamorphosis is also known as touch metamorphosis, where this type of metamorphosis is a metamorphosis that occurs when rocks are touched by hot magma around the magma chamber or intrusive rock bodies. An example of this thermal or touch metamorphosis is limestone turning into marble.

Dynamo's Metamorphosis

The next type of metamorphosis is dynamo metamorphosis or also known as pressure metamorphosis. This type of metamorphosis is a metamorphosis that occurs where there is rock that is exposed to pressure from tectonic events (on the earth's crust only occurs at the top) so that it will undergo metamorphosis. An example of this type of metamorphosis is in the fault plane a friction mirror or milonite flour is formed.

Regional Metamorphosis

The next type of metamorphosis is regional metamorphosis. Regional metamorphosis is also known as dynamic metamorphosis. Regional metamorphosis is a metamorphosis that affects a very wide area that occurs at the bottom of the earth's crust as a result of pressure throughout the formation of schist, mica, phyllite, and gneiss. Rocks can undergo metamorphosis only with or if they are at great depths below the earth's surface, experience high temperatures, and also experience great pressure caused by the enormous weight of the rock layers above and will disrupt the structure of the earth.. This regional metamorphosis tends to make the rock harder, and at the same time causes the formation of a foliated, schistos, or gneiss texture consisting of a mineral palanar arrangement. This causes plate or prismatic minerals such as mica and hornblende to have the longest axes that are parallel to each other. The main characteristic of metamorphic rocks that undergo this type of metamorphosis is the presence of a shiny color and also not fossilized.

Cataclastic Metamorphosis

Next there is a type of cataclastic metamorphosis. This cataclastic metamorphosis occurs as a result of mechanical deformation, such as when two bodies of rock slide past each other along a fault zone. Friction that occurs along the shear zone will generate heat, and the rock is mechanically deformed. The rock is then crushed and crushed as a result of the shift. This type of metamorphosis is not common confined to a narrow zone where a horizontal fault would occur.

Hydrothermal Metamorphosis

Next there is hydrothermal metamorphosis. Hydrothermal metamorphosis occurs when there are rocks that are changed at high temperatures and medium pressures due to hydrothermal fluids. This means that the rock is undergoing hydrithermal metamorphosis. This is common in basaltic rocks which generally lack hydrate minerals. This hydrothermal metamorphosis causes alteration to hydrate minerals rich in Mg – Fe such as talc, chlorite, serpentine, actinolite, tremolite, zeolite, and clay minerals rich in ore deposits are also often formed as a result of hydrothermal metamorphism.

Overlapping Metamorphosis

Then there is another type of metamorphosis, namely overlapping metamorphosis. Overlap metamorphosis will occur when sedimentary rocks are buried to a depth of several hundred meters, and temperatures greater than 300 degrees Celsius can develop in the absence of differential stress. New minerals grow, but the rock does not appear to be metamorphosed, the main mineral usually produced from this process is zeolite. This overlapping metamorphosis is an overlapping metamorphosis with diagnosis to some extent. and this metamorphosis can turn into regional metamorphosis with increasing temperature and pressure.

Those are some types of metamorphic processes that can occur in metamorphic rocks. The process of metamorphosis that occurs in this stone occurs because it is natural and occurs because of natural processes. The metamorphosis process that occurs in these rocks occurs due to natural processes involving certain elements such as water, wind, air temperature, sunlight, and so on. All that are involved in the metamorphosis process of this rock are natural materials or those that can be found in nature and cannot be made by humans.

The process of metamorphosis itself takes time. To be able to turn into a good stone and a perfect stone, the metamorphosis process itself requires supportive conditions, including the surrounding environment and time. The time required is also quite long and even quite long. Without human knowledge, these stones already exist and we ourselves are not aware of it. This is what is called a natural process.

Impact of Metamorphosis

The metamorphosis process experienced by these rocks not only produces certain stones, but also we will get certain impacts from this metamorphosis process.

When extraterrestrial material, such as types of solar system  types such as meteorites or comets, falls to earth, or in the event of a very large volcanic explosion, very high stresses can occur in the affected rocks.

These very high pressures produce minerals that can only be stable at very high pressures, such as SiO2 polymorphs such as coesite and stishophyte.

In addition they can also produce textures known as shock lamellae in mineral grains and also textures like or resembling broken cones in impacted rock.

That is the impact of the metamorphosis process. That's a little information about metamorphic rocks. Although not very complete but hopefully can provide useful knowledge.


Saturday, September 11, 2021

Sedimentary Rocks: Definition, Process, and Types

Sedimentary rocks"Sedimentary rocks" by thy is licensed under CC BY 2.0

Definition of Sedimentary Rock

Sedimentary rock is one type of rock which is formed as a result of compaction of sediment in the form of loose material. Sedimentary rocks or often also referred to as sediments are rocks that are formed from deposited materials carried by water or wind. There is another understanding of sedimentary rocks, namely rocks formed due to the process of petrification or lithification from the results of weathering processes and also soil erosion.which has been carried away by the current and then deposited. An expert, namely Hutton (1875) stated that this sedimentary rock is a rock formed by sediment consolidation, as loose material, which is transported to the depositional location by water, wind, ice and also gravitational avalanches, soil movements or landslides. Besides being formed from this, these sedimentary rocks are also formed by the evaporation of a solution of calcium carbonate, silica, salt, and other materials. This is what is called sedimentary rock.

Did you know that these sedimentary rocks are very numerous and widely spread on the earth's surface in this world? Even according to Tucker (1991), that 70% of the rocks found on the entire surface of the earth is a type of sedimentary rock. But the rock is only 2% of the volume of the entire earth's crust. This indicates that sedimentary rocks are spread very widely on the earth's surface, but their thickness is only relatively thin. The earth's crust is indeed composed of various kinds of materials, not only rocks but also layers of soil, sand, and others. And these rocks also include elements that make up the composition of the earth's crust . The rocks that make up the composition of the earth's crust are divided into various types and one of them is this sedimentary rock.

Sedimentary Rock Formation Process

 This sedimentary rock undergoes a process of compaction and also compaction of loose material (sediment) to become a solid sedimentary rock. This process is known as diagenesis. The diagenetic process itself can occur at atmospheric temperatures and pressures up to a temperature of 300 degrees Celsius and also a pressure of 1-2 kilobars which takes place from sediment experiencing burial to being lifted and also exposed again above the surface   of the  earth's atmosphere . Based on this, there are 3 types of diagnosis, namely:

  1. Eogenic diagnesa, namely the initial diagnesa that occurs in sediments below the water surface.
  2. Mesogenic diagnosis, namely the diagnesa that occurs when the sediment undergoes a deeper burial.
  3. Telogenic diagnosis, which occurs when sedimentary rocks are exposed back to the earth's surface due to uplift and erosion.

Those are the various types of diagnesa that occur in sedimentary rocks. Because there are various kinds of this diagnosis, the degree of compactness of these sedimentary rocks also varies or varies. Various kinds of compactness of these sedimentary rocks include:

  • Loose materials, namely those that are still in the form of deposits or sediments.
  • Solid or indurated. At this stage the consolidation of the material occurs in dry conditions. However, it will decompose when put into water.

Those are some types of compactness that occur in sedimentary rocks. After we study the compactness of sedimentary rocks, then we will learn about the texture of sedimentary rocks.

Sedimentary Rock Texture

As previously stated, these sedimentary rocks have a variety of textures. Sedimentary rock can be textured clastic or non-clastic. However, if the rock is very compact and if recrystallization or re-crystallization has occurred, then this sedimentary rock has a crystalline texture. Sedimentary rocks that have a crystalline texture generally occur in limestone and also silica-rich sedimentary rocks which are very compact and hard.

That's some information about sedimentary rocks that are widely available around us. As rocks that are widely found around us, these sedimentary rocks have many uses, especially for building materials or to decorate homes and buildings today. Thus information about sedimentary rocks that we can learn so that we can distinguish this type of rock from other rocks.

Types of Sedimentary Rocks

Sedimentary rocks are formed from igneous rock or other solid substances which are then eroded in certain places and then settle and eventually become hard. Sedimentary rocks are usually in the form of horizontal layers. Did you know that this type of sedimentary rock is still further divided into several types? The types of sedimentary rocks are classified according to several categories. Many experts categorize or classify these rock types with different amounts. Then, what are the types of these sedimentary rocks?

1. According to Pettijohn (1975), O'Dunn and Sill (1986) –  divide these sedimentary rocks based on their texture which is divided into two major groups, namely clastic sedimentary rocks and non-clastic sedimentary rocks.

Clastic sedimentary rocks are also called detritus, mechanical, exogenous sedimentary rocks which are sedimentary rocks consisting of clastics or crushed rocks that settle naturally or mechanically by their own gravity. This type of rock is formed as a result of reworking or reworkin from pre-existing rocks. The reworking process that occurs as rock formation includes weathering, erosion, transportation, and also redeposition or re-deposition. To support this process, several media are needed, namely water, wind, ice, and also the effects of gravity or its own weight. Especially for the latter media or this gravitational medium as a result of rock slides that have existed before.What we need to know from this type of rock group is that this rock group is fragmental or consists of grains or rock fragments so that it has a clastic texture. Examples of clastic sedimentary rocks include breccia, conglomerate, sandstone, and slab rock. Breccia is a sharp-angled gravel deposit that is still close to its place of origin. Conglomerate stones are gravel deposits whose corners are rounded (the corners that are far away are carried by the river). While sandstone is sedimentary rock derived from rock fragments measuring 1/16 to 2 millimeters.and also slate. Breccia is a sharp-angled gravel deposit that is still close to its place of origin. Conglomerate stones are gravel deposits whose corners are rounded (the corners that are far away are carried by the river). While sandstone is sedimentary rock derived from rock fragments measuring 1/16 to 2 millimeters.and also slate. Breccia is a sharp-angled gravel deposit that is still close to its place of origin. Conglomerate stones are gravel deposits whose corners are rounded (the corners that are far away are carried by the river). While sandstone is sedimentary rock derived from rock fragments measuring 1/16 to 2 millimeters.

Non-clastic sedimentary rock. Next we will discuss the types of non-clastic rock groups. This non-clastic rock is a type of sedimentary rock that is formed as a result of the evaporation of a solution or the deposition of material that is in the same place. The process of formation of this type of rock can occur by chemical, biological or organic processes, or a combination of the two, namely a combination of chemical and organic or biological. The process which is a combination of the two is called biochemistry. The process of rock formation that occurs biologically or organically is the formation process carried out by certain natural activities, namely by plants and animals. An example of this organic rock formation process is the formation of the home of marine animals or corals,accumulation of animal shells (fossils), and the burial of wood as a result of the land subsidence into the sea.

2. According to Sanders in 1981 and Tucker 1991 -  classify or divide these sedimentary rocks into four kinds, namely:


Detritus or clastic sedimentary rock

Chemical sedimentary rocks – Chemical sedimentary rocks are sedimentary rocks that are formed through chemical reactions, such as evaporation, precipitation, and concentration. Examples of these chemical sedimentary rocks are rock salt, gypsum rock, stalactites, and also stalagmites.

Organic sedimentary rocks – These organic sedimentary rocks are also known as sedimentary rocks of bodily origin. Organic sedimentary rock is sedimentary rock derived from the remains of living bodies or made by living organisms. This type of rock group can be broken down into two types, namely biomechanical sediments and biochemical sediments. Biomechanical sediments are deposits of the remains of living body parts that settle naturally under their own weight, for example, limestone, shells, numilites, and layered limestone. While biochemical sedimentary rocks are rocks that occur due to the deposition of limestone and silicium elements with living rocks.Examples of these rocks are limestone reefs or shellfish animal houses and also diatomaceous earth or the deposition of silicon elements due to the presence of carbon dioxide in the water which is absorbed by diatomaceous algae.

Volcanic clastic sedimentary rock. – Especially for this type of rock, it is a sedimentary rock that has a clastic texture with the main constituent materials derived from volcanic activity.

3. According to Graha (1987) –   This type of sedimentary rock is a sedimentary rock which is generally non-classical in texture. Graha divides these sedimentary rocks into four groups as well, namely:

  • Detritus sedimentary rock (clastic/mechanical)
  • Coal sedimentary rock (organic/vegetable)
  • Silica sedimentary rock, and
  • Carbonate sedimentary rock

Especially for this type of rock and also this silica sedimentary rock can be a clastic sedimentary rock or a non-clastic sedimentary rock. Then based on the composition of the main constituent, clastic sedimentary rocks or clastic textured, can be further divided into three kinds. Namely:

  • Siliciclastic sedimentary rock. This type of rock is a type of clastic sedimentary rock whose main constituent minerals are quartz and feldspar.
  • Then there are volcanic clastic sedimentary rocks. Volcanic sedimentary rock is one type of sedimentary rock with the main constituent materials derived from volcanic activity, such as glass, crystal, and/or lithic.
  • The last one is clastic carbonate sedimentary rock, also known as clastic limestone. This type of rock is a clastic sedimentary rock with the main constituent minerals being carbonate material (calcite).

Those are the types of clastic sedimentary rocks according to their main constituent composition. Next we will discuss the color of sedimentary rocks.

Sedimentary Rock Color

If we generally find that the rock is dark, i.e. black or slightly grayish, then this sedimentary rock has a slightly subdued or light color. This sedimentary rock has a distinctive color. The color of these sedimentary rocks is generally light or bright, such as white, yellow, or light gray. However, this sedimentary rock is not always bright or light in color. These sedimentary rocks have dark colors, namely dark gray to dark black, as well as red and brown. Thus this sedimentary rock has a variety of colors. The color variation of sedimentary rocks is caused by the composition of the constituent materials.


Igneous Rocks: Definition, Texture, Structure, Composition and Classification of Igneous Rocks

Obsidian 1"Obsidian 1" by James St. John is licensed under CC BY 2.0

Definition of Igneous Rock

Igneous rock or igneous rock (from Latin : ignis , "fire") is a type of rock formed from cooled and hardened magma , with or without a crystallization process , either below the surface as intrusive (plutonic) rock or above the surface as rock. extrusive (volcanic). This magma can come from semi-molten rock or rock that is already present, either in the mantle or crust. Generally, the melting process occurs by one of the following processes: temperature rise , pressure drop, or a change in composition. More than 700 types of igneous rock have been described, most of which form beneath the surface of the Earth's crust .

According to scholars such as Turner and Verhoogen (1960), F. F Groun (1947), Takeda (1970), magma is defined as a naturally occurring viscous, incandescent, viscous silicate liquid, with a high temperature between 1,500–2.5000C and mobile (can move). and is found in the lower crust of the earth. In the magma there are several soluble, volatile materials (water, CO2, chlorine, fluorine, iron, sulfur, etc.) found in igneous rocks.

When magma experiences a decrease in temperature due to travel to the earth's surface, minerals will form. This event is known as the scattering event. Based on the crystallization of silicate minerals (magma), by NL. Bowen compiled a series known as Bowen's Reaction Series.

Texture of Igneous Rock

Texture is defined as a condition or a tight relationship between minerals as part of a rock and between minerals with a glass mass that forms the foundation mass of the rock.

The texture of igneous rocks is generally determined by three important things, namely:

Crystallinity

Crystallinity is the degree of crystallization of an igneous rock at the time the rock was formed. Crystallinity in its function is used to indicate how much is in the form of crystals and which is not in the form of crystals, but it can also reflect the speed of magma freezing. If magma continues to freeze slowly then the crystals are coarse. Meanwhile, if the freezing continues quickly then the crystals will be smooth, but if the cooling continues very quickly then the crystals are amorphous.

In its formation, there are three classes of degrees of crystallization, namely:


  • Holocrystalline, i.e. igneous rock where everything is composed of crystals. The holocrystalline texture is characteristic of plutonic rocks, which are microcrystalline rocks that have frozen near the surface.
  • Hypocrystalline, ie when some rocks consist of glass mass and some consist of crystal mass.
  • Holohyaline, i.e. igneous rock which is all composed of glass mass. Most holohyaline textures are formed as lava (obsidian), dike and sill, or as facies smaller than rock bodies.

Granularity

Granularity is defined as the grain size (size) in igneous rocks. There are two types of grain size textures known, namely:

  • Phaneric/phanerocrystalline

Most of the crystals of this group can be distinguished from each other megascopically with the naked eye. The crystals of this faneric type can be divided into:

  • Fine, if the grain diameter is less than 1 mm.
  • Medium (medium), if the grain diameter is between 1-5 mm.
  • Coarse, if the grain diameter is between 5-30 mm.
  • Very coarse, if the grain diameter is more than 30 mm.

Afanitik

Most of the crystals of this group are indistinguishable with the naked eye, so a microscope is needed. Rocks with an aphanitic texture can be composed of crystal, glass or both. In microscopic analysis can be distinguished:

  • Microcrystalline, if the minerals in igneous rocks can be secured with the help of a microscope with a grain size of about 0.1 – 0.01 mm.
  • Cryptocrystalline, when the minerals in the igneous rock are too small to be secured even with the aid of a microscope. The grain size ranges from 0.01 to 0.002 mm.
  • Amorphous / glassy / hyaline, if the igneous rock is composed of glass.

Crystal Form

Crystal form is the nature of a crystal in rock, so it is not a rock property as a whole. From a two-dimensional view, there are three forms of crystals, namely:

  • Euhedral, if the boundary of the mineral is the original form of the crystal member.
  • Subhedral, when some of the crystal boundaries are no longer visible.
  • Anhedral, if the mineral no longer consists of original crystals.

From a three-dimensional perspective, four crystal forms are known, namely:

  • Equidimensional, if the three-dimensional crystal form is the same length.
  • Tabular, if the two-dimensional crystal form is longer than one of the other dimensions.
  • Prismatic, if the crystal form in one dimension is longer than the other two dimensions.
  • Irregular, if the crystal form is chaotic.

Relationship Between Crystals

The relationship between crystals or also called the relationship is defined as the relationship between crystals / minerals with one another in a rock. Broadly speaking, relations can be divided into two,

Equigranular

Equigranular is, if the relative size of the crystals that make up the rock are of the same size. Based on the ideality of the crystals, therefore equigranular is divided into three, namely:

  • Panidiomorphic granular, ie when most of the minerals consist of euhedral minerals.
  • Hipidiomorphic granular, ie when most of the minerals consist of subhedral minerals.
  • Allotriomorphic granular, ie when most of the minerals consist of anhedral minerals.

Inequigranular

Inequigranular is if the size of the crystal grains as rock-forming is very different. The large mineral is called the phenocryst and the other is called the ground mass or matrix which can be mineral or glass.

Structure of Igneous Rock

Structure is the macro appearance of rocks which includes the location of a clear / general layer of rock layers. Most igneous rock structures can only be seen and observed in the field, for example:

  • Pillow lava or pillow lava, which is a very typical structure of underwater volcanic rock, forms a pillow-like structure.
  • Joint structure, is a structure characterized by the presence of joints that are arranged regularly perpendicular to the direction of the current. While the structure that can be seen and observed in rock samples (hand speciment samples), namely:
  • Massive, that is, if it does not show the presence of currents, traces of gas (does not indicate the presence of holes) and does not indicate the presence of other fragments embedded in the igneous rock body.
  • Vesicular, which is a structure with holes caused by the release of gas at the time of magma freezing. The holes show a regular direction.
  • Scoria, which is the same structure as the vesicular structure but the holes are large and show a chaotic direction.
  • Amygdaloidal, namely the structure where the gas holes have been filled by secondary minerals, mostly silicate or carbonate minerals.
  • Xenoliths, namely structures that show the presence of other rock fragments / fragments that enter the intrusive rock.
  • Most igneous rocks are without structure (massive), while the structures that are present in igneous rocks are made by joints or fractures and magma freezing, for example: columnar joints and sheeting joints.

Mineral Composition of Igneous Rock

To determine the mineral composition of igneous rock, it is enough to use the color index of the crystalline rock. On the basis of the color of minerals as a constituent of igneous rocks can be grouped into two, namely:

  • Felsic minerals, which are light colored minerals, mainly consist of quartz, feldspar, feldspathoid and muscovite minerals.
  • Mafic minerals are dark colored minerals, especially biotite, pyroxene, amphibole and olivine.

Igneous Rock Classification

Igneous rocks can be classified according to the manner in which they occur, the content of SiO2, and the color index. Thus, different rock names can be determined, even though they are in the same rock type, according to their classification basis.

Classification by way of occurrence

According to Rosenbusch (1877-1976) igneous rocks are divided into:

Effusive rock, for igneous rock that forms on the surface.

Dike rock, for igneous rock that forms near the surface.

Deep seated rock, for igneous rock deep in the earth. By WT Huang (1962), this rock type is called plutonic, while effusive rock is called volcanic rock.

Classification based on SiO2 

According to (CL Hugnes, 1962), namely:

Acid igneous rock, if the SiO2 content is more than 66%. For example, rhyolite.

Intermediate igneous rock, if the SiO2 content is between 52% - 66%. For example, dasit.

Alkaline igneous rock, if the SiO2 content is between 45% - 52%. For example, andesite.

Ultra-alkaline igneous rock, when the SiO2 content is less than 45%. For example, basalt.

Classification by color index

According to (SJ Shand, 1943), namely:

Leucoctaris rock, if it contains less than 30% mafic minerals.

Mesococtic rock, if it contains 30% - 60% mafic minerals.

Melanocratic rock, if it contains more than 60% mafic minerals.


Meanwhile, according to SJ Ellis (1948) also divides igneous rocks based on their color index as follows:

Holofelsic, for igneous rocks with a color index of less than 10%.

Felsic, for igneous rocks with a color index of 10% to 40%.

Mafelsic, for igneous rocks with a color index of 40% to 70%.

Mafic, for igneous rocks with a color index of more than 70%.

Types of igneous rock

Igneous rocks can be divided into 3 categories:

  • Deep igneous rocks, for example: granite, diorite, and gabbro
  • Igneous rock alley / middle, for example: porphyry granite
  • External igneous rocks, for example: andesite, obsidian, and basalt

Friday, September 10, 2021

Deuteromycota: Definition, Characteristics, Reproduction, Way of Life, Examples and Their Role

 Definition of Deuteromycota

Deuteromycota fungi are fungi that reproduce by conidia and have no known sexual stage. Neither ascus nor basidium were found so they were not included in the Ascomycota or Basidiomycota fungi class. Therefore, this fungus is an imperfect fungus (fungi imperfecti).

In addition to conidia, asexual reproduction of Deuteromycota fungi can also be carried out by forming blastospores (bud form) and arthrospores (spore formation with hyphal threads).

Thus, several types of fungi whose generative reproductive organs are not yet known are included in the Deuteromycota division. Deutermycota or  the imperfect fungi  do not undergo sexual reproduction or they exhibit an asexual stage ( anamorph ) than fungi that have a sexual stage ( teleomorph ).

Deuteromycota fungi resemble Ascomycota (simple septa). So, this group of mushrooms can be called a "trash basket", a temporary place to accommodate the types of mushrooms whose status is not yet clear. If in the next study a method of sexual reproduction is found, then a type of fungus belonging to the Deuteromycota will be grouped into the Ascomycota division or the Basidiomycota division.

For example, the fungus  Monilia sitophila  (oncom fungus), before it was known for its sexual reproduction was classified as Deuteromycota, but now that it is known for its sexual reproduction by producing ascospores in the ascus (perithesium), it is grouped into Ascomycota and renamed  Neurospora sitophila  or  Neurospora crassa .

But there are still experts who classify the Penicillium and Aspergillus fungi into Deuteromycotina on the grounds that the conidium level is so clear and familiar, even though the sexual level is well known.

Characteristics of Deuteromycota

In general, the characteristics or characteristics of fungi belonging to the division Deuteromycota include the following.

■ multicellular (multicellular) that form hyphae not insulated, but some types are single-celled organisms that form pseudomiselium (pseudo mycelium) on the environmental conditions are favorable.  

■ Most of the microscopic (can not be observed with the naked eye).  

■ The cell walls made of chitin substance.  

■ In certain types found hyphae insulated with a nucleated cell, but mostly multinucleated ..  

■ Formed vegetative spores and unknown so that the mating phase called imperfect fungi or imperfekti.  

■ Breed with spores asexually through fragmentation and konidium are unicellular or multicellular. While sexual reproduction is not yet known.  

■ Many destructive or cause disease in farm animals, humans and crops.  

■ Living saprophyte or parasite. 

■ Usually berhabitat in damp areas.  

The Deuteromycota's Way of Life

All fungi belonging to this artificial division reproduce asexually with conidia. Conidia are formed at the ends of the conidiospores, directly on the free hyphae. Some species live on leaves and plant debris that sink to the bottom of a fast-flowing river.

Several other groups are parasitic on protozoa and other small animals in various ways. Several species are also found in ant and termite nests.

Some parasitic fungi in small animals develop an  unbranched body  in their victim's body, then slowly absorb nutrients until the victim dies. After that the fungus produces a chain of spores that may attach to or be eaten by other animals that will become victims.

Another way is to catch prey with hyphae that can pierce, by hitchhiking and attaching to the amoeba. One group of soil-dwelling fungi is capable of catching nematode worms by forming  hyphae rings  or  hyphal loops .

The size of the hyphae ring is smaller than the size of the nematode body and is pointed at both ends. When a nematode inserts its head into a hyphal ring, the worm tends to try to get out by moving forward, not backward, so that the worm gets stuck in the fungal hyphae coil.

After successfully ensnaring its victim, the fungus then forms a haustoria that grows to penetrate into the worm's body and digest it.

Deuteromycota Reproduction Method

■ Asexual reproduction occurs by producing conidia or produce specialized hyphae called conidiophores.  

■ Despite having no sexual reproduction, but genetic recombination can still occur, so called by paraseksualitas. This parasexual cycle is the process of sending genetic material without going through meiotic division and the development of sexual structures.

Examples of Deuteromycota and Their Role

In humans, fungi belonging to the division Deuteromycota commonly cause disease. Examples are as follows.

■ Epidermophyton floocosum  cause athlete's foot disease (water flea).  

■ Microsporum sp.  and  Trichophyton sp.  cause ringworm or tinea versicolor. Because they live on the skin, the two fungi are often referred to as dermatophytes .  

■ Candida albicans  is a microscopic fungus that has yeast-like body shape, but the nature of his life is a parasite. The disease it causes is a vaginal discharge that occurs due to an infection in the vagina. 

■ Tinea versicolor  causes phlegm.  

■ Melazasia fur-fur , causing phlegm.  

■ Trychophyton tonsurans , cause dandruff on the head.  

Deuteromycota also have several members that cause disease in plants, including the following.

■ Sclerotium rolfsie  is a fungus that causes rot in plants cultivation.  

■ Helminthosporium oryzae  is an example of a parasitic fungus that can destroy sprouts and fruit and can cause black spots on the leaves of the host (rice and corn).  

■ Alternaria  parasite on potato. 

■ Fusarium  parasites on tomato plants and cotton.  

■ Diplodia  parasite on maize.  

■ Verticillium  attacking seedlings.  

■ Colletrichum  parasites in the red onion.

Basidiomycota: Definition, Characteristics, Structure, Reproduction, Examples and Roles

Basidiomycota type"Basidiomycota type" by gailhampshire is licensed under CC BY 2.0

Definition of Basidiomycota

The term "basidiomycota" comes from the Greek, namely from the word  basidium,  which is a diploid stage in the life cycle of Basidiomycota which is shaped like a club. In general, this fungus is an important saproba. Its activity is to decompose lignin polymers in wood and various other plant parts.

The Basidiomycota division is often referred to as  the club fungus  or commonly known as mushrooms (fungus or  mushrooms ). This fungus reproduces sexually by forming basidia which then produce basidiospores in the fruiting body called basidioma or basidiocarp.

These basidia can develop in the form of gills, pores, such as teeth, or other structures. Hyphae of Basiomycota are generally dikaryotic (binucleate, with 2 nuclei) and sometimes have flanking relationships. The cells are separated by complex septa.

Its members are mostly macroscopic fungi. This group has an insulated mycelium and has long fruiting bodies (basidiocarps), in the form of sheets, which are tortuous or round. These fungi generally live saprophytes and parasites, generally reproduce asexually with conidia.

If you see people using mushrooms as food, what is meant is "mushroom" or kenthos mushrooms ( puffball ). Both include the very popular Basidiomycota, in addition to several other types of mushrooms that are commonly cooked as food ingredients.

How to Live Basidiomycota Fungi

In general, Basidiomycota live as saprobes (decomposers) the remains of dead organisms. Basidiomycota live in soil containing organic waste, on dead logs, or in haystacks.

Compared to other types of fungi, Basidiomycota is the best decomposer of complex lignin polymers. Lignin is a component of wood. Basidiomycota can also live in mutualism symbiosis with plant roots by forming mycorrhizae, but some are parasitic on other organisms.

Characteristics of Basidiomycota

In general, the characteristics or characteristics of fungi belonging to the division Basidiomycota include the following.

■ multicellular (multicellular).  

■ Is a macroscopic fungi, can be seen directly, and has a large size.  

■ Characteristically saprophytic or parasitic on other organisms and mycorrhizae.  

■ All members of the Basidiomycota division berhabitat on land.  

The hyphae are septate, containing a haploid nucleus with a clamp connection .  

■ Have a fruiting body shaped like an umbrella that consists of the trunk and hood. At the bottom of the hood, there are sheets (slats) which are where the basidium is formed. The fruiting body is called the basidiocarp.  

■ The shape of the fruit body varies, there is such as umbrellas, balls, boards, sheets berleku grooved and so forth.  

■ fruiting bodies called basidiokarp, consists of interwoven hyphae insulated and dikaryotic (each core pair).  

The color of the fruiting body varies (colorful).  

■ Most can be consumed, but there are some fungi can also be deadly. Some members of the genus Amanita contain a very deadly poison. Some types of Basidiomycota can also harm plants, for example causing death in field crops. Examples of other Basidiomycota, namely Auricularia polytricha (ear fungus),  Volvariella volvaceae  (edible mushroom), and  Ganoderma.

■ Reproduction sexually by forming and seldom do basidiospora and asexual reproduction is by fragmentation of the hyphae.  

■ basidiospores formed outside basidium.  

■ Each basidium containing 2 or 4 basidiospora, respectively one and haploid nuclei. All basidiospores gather to form a fruiting body (basidiocarp).  

■ Basidiokarp often form a rod-like structures called the  stalk  and like an umbrella called hood.  

■ It has three types of mycelium are as follows.

Primary mycelium : produced from newly grown spores. At first this mycelium is multinucleated, then septa are formed which contain one nucleus and are haploid.

Secondary mycelium : resulting from plasmogamy or the union of two corresponding hyphae. This mycelium has two nuclei, each of which is haploid.

Tertiary mycelium : consists of secondary mycelium that has united to form a kind of network, for example to form basidiocarp and basidiophores.

Body Structure of Basidiomycota

Basidiomycota fungi are characterized by having a basidium. This group of fungi is known for its fruiting bodies that are clearly visible on the surface of the soil or other substrates. Fruiting bodies vary in shape, some are like umbrellas, balls or boards. For example, the edible mushroom ( Volvariella volvacea ) with an umbrella-shaped fruiting body.

In general, the fruiting body has 4 parts, namely as follows.

■ fruiting bodies (stipe)  is an upright growing mycelium mass.  

■ Hood (pileus)  is a part that is supported by stipe. When young, the pileus is covered by a membrane called the  velum universale  which will rupture at maturity.  

■ volva  is the rest of the wrappers contained in the bottom of the stalk.  

️lamella  is the lower part of the hood, blade-shaped, and arranged on the sheet.

️annulus , a ring encircling the stem position.

■ Gill   was part under the hood in the form of sheet-shaped blades such as the gills where basidium produce basidiospores as generative reproduction.

The fruiting bodies of Basidiomycota fungi are called basidiocarps, consisting of a network of insulated and dikaryotic hyphae (each cell nucleus is in pairs). At the time of formation of basidiospores, the ends of the hyphae swell to form a basidium in which the fusion of two haploid nuclei occurs into one diploid nucleus, followed by meiotic division which produces 4 haploid nuclei.

Furthermore, the basidium forms four protrusions (sterigmata) containing protoplasm and the four haploid nuclei will each fill each protrusion and form four haploid basidiospores.

How to Reproduction Basidiomycota

Basidiomycota can reproduce by two methods, namely generative (sexual) and vegetative (asexual). So what are the processes and stages? Here is the explanation.

1. Sexual Reproduction Basidiomycota

The stages of sexual or generative reproduction of Basidiomycota are as follows.

1. Spores have haploid +  and haploid nuclei -  grow into +  hyphae and hyphae -  .

2. Hyphae +  and hyphae –  will fuse to form dikaryotic hyphae (2 nuclei).

3. Dikaryotic hyphae grow into mycelium and eventually form a fruiting body (basidiocarp).

4. The ends of the hyphae in the basidiocarp swell (called the basidium) and the two haploid nuclei become one diploid nucleus.

5. The diploid nucleus divides by meiosis into 4 haploid nuclei. Basidium forms 4 protrusions and each protrusion is filled with 1 haploid nucleus which will develop into spores called basidiospores.

6. Mature basidiospores will be released from the basidium and if they fall in a suitable place will grow into hyphae.

2. Basidiomycota Asexual Reproduction

Asexual reproduction occurs by forming conidiospores. Conidia are spores produced by forming a transverse bulkhead at the tip of the hyphae or by differentiation to form many conidia. Mature haploid hyphae will produce conidiophores (conidia stalks).

At the tip of the conidiophores, spores are formed. Then the spores will be blown away by the wind. If the environmental conditions are favorable, the conidia will germinate into haploid hyphae.

Basidiomycota Life Cycle

The spores produced by basidium (basidiospores) are haploid and grow to form insulated hyphae, each with one nucleus, some as + (male) hyphae and some -  (female) hyphae  . If the two meet, there will be plasmogamy / mixing of plasma cells and a hyphae cell with dikaryotic / two nuclei will be formed.

The hyphae will continue to develop to form mycelium which is still dikaryotic, so that a basidiocarp fruiting body that looks like an umbrella will be formed. This basidiocarp will produce a basidium contained in a layer called the  hymenium .

In that place, karyogamy will occur, namely the union of two nuclei into one and this nucleus will undergo meiotic division to form 4 haploid spores called basidiospores, and so on.

Examples and Roles of Basidiomycota

Most of the fungi that we see in everyday life belong to the class Basidiomycota. Currently, approximately 12,000 species of Basidiomycota are known and none of them causes infectious disease in humans. Most Basidiomycota are saprobes and parasites on plants and insects.

Some types of Basidiomycota are edible and safe, but many species are found to produce mycotoxin toxins that can cause death if ingested. Mushrooms that are cultivated because they have economic value are called mushrooms. The following are some examples of Basidiomycota fungi and their role in human life.

Examples of beneficial Basidiomycota Fungi

■ Volvariella volvacea (mushroom), This mushroom has a fruiting body shaped like an umbrella, consisting of sheets (blades), which contain a basidium. The fruit body is reddish white. This mushroom is a source of protein, high in calories, but low in cholesterol. Because it has a high economic value, this mushroom is widely cultivated.

■ Auricularia polythrica (mushroom) is a saprophytic fungus on dead wood. The fruiting body is shaped like an ear (ear), red-brown in color. It tastes good and can be eaten like a vegetable. This mushroom is now widely cultivated.

■ The oyster mushroom (Pleurotus sp.) , Wood mushrooms or oyster mushrooms. This mushroom is good for consumption, a good habitat in an environment that contains a lot of lignin and cellulose. This mushroom has been widely cultivated with sawdust medium.

■ Mushroom shitake  is a fungus that commonly manufactured in China and Japan, living in a log.  

■ Lentinous edodes , this fungus species other than human consumption can also be used as medicine.  

■ Amanita caesarina , Unlike poisonous Amanita muscaria, mushroom Amanita Caesarea that bright orange has a delicious flavor and is a favorite food of the Roman emperor named Nero.

Examples of harmful Basidiomycota Fungi

■ Amanita phalloides  

Amanita phalloides is a member of the Amanitaceae family. Amanita, a beautiful fungus, but also a member of the list of the deadliest fungi on earth, contains enough poison to kill an adult with just a piece of her body. This fungus lives as a saprophyte in livestock manure, has a fruiting body shaped like an umbrella.

■ stem rust (rust)  

This fungus lives as a parasite on the leaves of grasses (Graminae), its body is macroscopic, it does not have a fruiting body, and its spores are brownish red like rust.

■ corn smut , this fungus is parasitic on corn, attacking sukam leaves, cobs, and stalks tassels. The most striking feature if corn plants are attacked by this fungus is the presence of some corn grains on the cobs that are much larger than normal size.  

■ Calvatia gigantea ,  known as the  giant puffball , has a very large fruit body with a diameter and 1 meter, so it can issue totaling trillions of spores.  

■ Amanita muscaria  , these fungi produce toxins that can kill flies muskarin. Lives on manure.

■ Ganoderma applanatum  (fungus) This fungus causes damage to the wood.  

■ Ganoderma pseudoferreum , this fungus causes root rot on cocoa, coffee, tea, rubber and other plantation crops.  

■ stem rust , cause disease in sugarcane and corn.  

■ Ustilago scitamanae  parasite on the plant leaf Graminae.  

■ Puccinia arachidis  , parasitic on peanut plants.

■ Phakospora pachyrhizi  , parasitic on soybeans.

■ Amanita verna  toxic, live in the land of white or red.  

■ Exobasidium vexans  live parasites on the tea plant.