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Diterbitkan olehucu wandi somantri sukardjo Telah diubah "6 tahun yang lalu
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Algae: Overview and Importance for Earth’s Atmosphere
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Earth’s Atmosphere: Not Much of It Mass Atmosphere = 5.2 x 10 18 kg Mass Oceans = 1.4 x 10 21 kg Mass Earth = 6.0 x 10 24 kg Live Biomass = 1 x 10 15 kg Carbon Dioxide = 3 x 10 15 kg Trunover Time for carbon dioxide = 5 years in atmosphere, centuries in oceans
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Carbon dioxide cycles between low values in summer and higher values in winter in the Northern Hemisphere due to seasonal differences in photosynthesis. Annual input from fossil fuels and deforestation: 3 x 1013 kg carbon dioxide. Half accumulates in the atmosphere, rest is absorbed in oceans, leading to acidification. Pre-industrial carbon dioxide level was 280 ppm, now 380 ppm.
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Early Earth Atmosphere: No Oxygen Lots of Carbon Dioxide, Methane, Water Vapor, Hydrogen
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Cyanobacteria and Oxygenic Photosynthesis About 3 Billion Years Ago. Water is the electron donor. CO 2 + H 2 O CH 2 O + O 2
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Oxygenic photosynthesis is complicated. It requires two photosystems and is thought to have arisen only once in the course of evolution.
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Modern Stromatolites Fossil Stromatolite (2.5 Billion Years Old) Banded Iron Formation Oxygen Was A Poison to Early Life Forms on Earth. Took about 1 billion years before oceans and atmosphere were fully oxygenated
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Oxygen in the air allowed the evolution of eucaryotes and aerobic respiration, finally leading to the world’s life forms present today.
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Ozone in the upper atmosphere (derived from O 2 ) protects against the splitting H 2 O to H and OH, with H escaping to space. Earth has lost about 25% of its water while water is nearly all gone on Venus and Mars. Oxygen also produced the ozone shield which protects water in the upper atmosphere from boiling away as hydrogen
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Greenhouse Gasses: Water Vapor Carbon Dioxide* Methane* Nitrous Oxide* *Increasing Due To Human Activity
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Evolution of the modern algae orders. 60 Ma 1500 Ma
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600 Ma to present – evolution of animal kingdom
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SNOWBALL EARTH 1 st - 2200 MYA 2 nd – 850 MYA
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Plate tectonics provides a resupply of carbon dioxide to the atmosphere
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Diatoms Grasses 50 MYA Diatoms and Grasses Reduce Carbon Dioxide to Very Low Levels
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Evolution and impacts of algae on the atmosphere continue today…
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In this course we emphasize the ecology and biology of the algae rather than the taxonomy. Main groups we will cover: Cyanobacteria (blue-green algae) Green Algae Red Algae Brown algae – brown seaweeds, kelps, diatoms Dinoflagellates Coccolithophores Others
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Cyanobacteria Cell Structure
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Nostoc filaments with N 2 -fixing heterocysts Nostoc colony
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Ceramium – filamentous red seaweed
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Porphyridium – Unicellular Bangean Red Algae
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Chlamydomonas
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Ulva Enteromorpha Monostroma
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Diatoms Heterokont in sexual stage
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Desmokont Dinokont Dinoflagellates Red-Tide Forming Prorocentrum Lingulodinium
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Red Tides
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Coccolithophores Haptophytes w/ two smooth flagella and a coiled hapto- nema Emiliania huxleyi Ca + 2HCO3 ---> CaCO3 + H2O + CO2
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