life cycle of anoplogaster?
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i get a cycle but i dont call it anoplogaster
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http://ccma.nos.noaa.gov/images/biogeo/conch.gif
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There is this lifeform which I can't remember the name of, but it is the most interesting because it can turn into 2 different species of lifeform, it can be a type of fungus and then it can turn into a worm-like creature and crawl away...
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Clown fish, anemone fish
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The life cycle of the ant consists of four stages: egg, larva, pupa, and adult. Fertilized eggs produce female ants (queens, workers, or soldiers); unfertilized eggs produce male ants. \nEgg: Ant eggs are oval shaped and tiny (they are on the order of 1 mm long, but the queen's egg is many times larger). \n\nLarva: The worm-like larvae have no eyes and no legs; they eat food regurgitated by adult ants. The larvae molt (shed their skin) many times as they increase in size. \n\nPupa: After reaching a certain size, the larva spins a silk-like cocoon around itself (against a solid object, like the wall of the chamber) and pupates. During this time the body metamorphoses (changes) into its adult form. \n\nAdult: The pupa emerges as an adult. The entire life cycle usually lasts from 6 to 10 weeks. Some queens can live over 15 years, and some workers can live for up to 7 years.
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Growth of algae I believe.
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See this link\n\nhttp://us.badm.washington.edu/yalch/Research/atmosphe.htm
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http://dev.biologists.org/cgi/content/full/130/17/4123?ck=nck
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a person throughout their life cycle.  Baby, adult, old age
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Reproduction\n\nUnder favorable conditions amebas divide by binary fission (splitting) to produce two daughter amebas, the nucleus dividing by mitosis. When an ameba is divided artificially, the portion containing the nucleus forms a new cell membrane and continues as a whole animal, while the other portion lives only as long as its present food supply lasts, ultimately dying, since it cannot ingest food or reproduce. If conditions are unfavorable, e.g., in the absence of food and water, amebas secrete a firm protective covering and encyst until conditions are again favorable to active division.
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http://www.flmnh.ufl.edu/natsci/herpetology/brittoncrocs/csp_amis.htm\n\ntypically 1 year
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algal production is the major source of energy for the anemone,  but they also hunt for food.  They are capable of travelling accross the reef on their 'foot'. they appear to have indefinate lifespans.  http://www.reefs.org/library/article/r_toonen8.html \nhttp://www.reefs.org/library/talklog/r_talukdar_102697.html
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# Anoxic autotrophs: Obtain hydrogen from chemicals such as sulfur.\n[[[[[[[[[[[[[[[[[[[[[[[[[[[[[[[[[[Dead Zones are areas where the bottom water (the water at the sea floor) is anoxic, meaning that it has very low (or completely zero) concentrations of dissolved oxygen.]]]]]]]]]]]]]]]]]]]]]]]]]\nDead Zones are areas where the bottom water (the water at the sea floor) is anoxic, meaning that it has very low (or completely zero) concentrations of dissolved oxygen. These dead zones are occurring in many areas along the coasts of major continents, and they are spreading over larger areas of the sea floor. Because very few organisms can tolerate the lack of oxygen in these areas, they can destroy the habitat in which numerous organisms make their home.\n\nThe cause of anoxic bottom waters is fairly simple: the organic matter produced by phytoplankton at the surface of the ocean (in the euphotic zone) sinks to the bottom (the benthic zone) where it is subject to breakdown by the action of bacteria, a process known as bacterial respiration. The problem is, while phytoplankton use carbon dioxide and produce oxygen during photosynthesis, bacteria use oxygen and give off carbon dioxide during respiration. The oxygen used by bacteria is the oxygen dissolved in the water, and that’s the same oxygen that all of the other oxygen-respiring animals on the bottom (crabs, clams, shrimp, and a host of mud-loving creatures) and swimming in the water (zooplankton, fish) require for life to continue.\n\nThe "creeping dead zones" are areas in the ocean where it appears that phytoplankton productivity has been enhanced, or natural water flow has been restricted, leading to increasing bottom water anoxia. If phytoplankton productivity is enhanced, more organic matter is produced, more organic matter sinks to the bottom and is respired by bacteria, and thus more oxygen is consumed. If water flow is restricted, the natural refreshing flow of "oxic" waters (water with normal dissolved oxygen concentrations) is reduced, so that the remaining oxygen is depleted faster.\n\nMany of the areas where increasing bottom water anoxia has recently been observed are near the mouths of major river systems. While Satellite images can’t see the bottom of the ocean, they can see the surface, where sediments from rivers mix with ocean waters. The images shown here are Satellite images (SeaWiFS) observations of the Mississippi River delta, the Yangtze River mouth in China (The Yangtze River mouth is not currently identified as an area with an associated dead zone, but such conditions could develop there in the future), and the Pearl River mouth in China, near Hong Kong.\n\nSeaWiFS can also observe areas where water flow is restricted, such as the Baltic Sea in Europe. The image on the left features Denmark after strong storms caused flooding and increased sediment suspension in the Baltic. On the right is an overview of the Baltic Sea, including a plankton bloom in the Skagerrak just north of Denmark.\n\nThe apparent cause of the creeping dead zones is agriculture, specifically fertilizer. While fertilizer is necessary to foster bumper agricultural crops, it also runs off the fields into the streams and rivers of a watershed. When the fertilizer reaches the ocean, it just becomes more nutrients for the phytoplankton, so they do what they do best: they grow and multiply. Which leads to more organic matter reaching the bottom, more bacterial respiration, and more anoxic bottom water.\n\nThese effects can be magnified by catastrophe. When the heavy rains of Hurricane Floyd caused extensive flooding in North Carolina in September 1999, the heavy load of nutrients (from dead animals, flooded animal waste ponds, and numerous other sources) reached the sounds that lie between the coast and the Outer Banks, oxygen levels in the water plummeted. The picture at the top of the page shows the heavy load of sediments flowing into Pamlico Sound. SeaWiFS captur
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Sure, ask a question with no answer.;-) \nThere is currently no information available about the breeding behavior of this species according to University of Texas Austin.  Because it is a cave salamander it is likely that there is no actual breeding season for this species. In a cave environment most or all seasonal cues such as changes in day length, or temperature are absent. \n\nBelow is a description of what is known about the breeding behavior of the Texas Blind Salamander, which are closely related taxonomically, geographically, and in habitat to the Cascade Caverns Salamander. It seems to be the only info available for any of the cave salamanders in TX. It's probably fair to speculate that their breeding strategies are similar or even the same.\n\n\nLittle is known about the reproduction of Eurycea (Typhlomolge) rathbuni. The species is known to be acyclic with females maturing and reproducing throughout the year, unresponsive to seasonal cues. This breeding cycle is typical of many cave dwelling species (Lofts 1974). Breeding of this species has been observed in the laboratory. The females assumes an active role in stimulating the male to mate. Her behavior is characterized by rubbing her chin along the male's back. If this fails to stimulate the male then she may scratch at him or fan her tail at him. She may even resort to nipping at his sides if he further ignores her advances. The male will deposit a spermatophore on a rock or substrate and the female will then pick it up with her cloaca (Bechler 1988).
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I found it on the web site. Scroll to the bottom of the page.\n\nhttp://scitec.uwichill.edu.bb/bcs/courses/Ecology/BL21C/ECOL2453_sc/Seasonal_communities.html
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About one week depending on the species.
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Salps are gelatinous, mostly transparent, and cylindrically shaped. They vary in size from a few millimetres at birth  up to about 10cm. One species is known to reach a few meters. Individual salps form a colony during the sexual phase of their lifecycle. The colony is long and chain-like in some species and  wheel-like in others.\nSalps filter food particles by pumping seawater in the mouth opening and out the atrial opening using muscle contractions. This pumping action gives animals propulsion, too so swimming and feeding occur at the same time.\nSalps have a complex lifecycle alternating between a sexual and asexual form. Sexual forms are called aggregates because they form a colony while asexual forms are solitary. All females have one or two eggs when released by a solitary parent. Mating occurs with larger male aggregates and embryos grow inside an aggregate body by being nurtured through a placenta. When embryos mature, they are released and the mother aggregate becomes male. Released embryos grow to be mature solitaries that asexually reproduce ‘stolons’ - buds of young aggregates.\nPretty wierd, huh? They look like jelly fish. And no, no backbones...!!