L10 - Nutrients and biogeochemical cycles Flashcards
What are phytoplankton important in?
Carbon and other biogeochemical cycles in marine and atmospheric systems. Overall, the ocean is a carbon ‘sink’: it takes up more carbon from the atmosphere than it gives up.
Summary of the carbon cycle?
There are many important volatile gasses released from the ocean to the atmosphere that impact cloud formation, albedo etc. Before the industrial revolution, the ocean was a source of CO2, now the oceans act as a carbon sink - equilibrium.
What is plankton greek for?
Drifter
What are biogeochemical cycles?
Cycles of nutrients or minerals that involve biology, geology and chemistry.
Biogeochemical cycles - POC (and or TC) - DOC?
Particulate Organic Carbon (>0.2 microns is a particle, if less, its Dissolved Organic Carbon)
Biogeochemical cycles - PON - DON?
Particulate (Dissolved) Organic Nitrogen
Biogeochemical cycles - POP (DOP)?
Particulate (Dissolved) Organic Phosphorus
Biogeochemical cycles - DIP (Pi Phosphate) DIP?
Dissolved In-organic Phosphorus
Biogeochemical cycles - DCM?
Deep Chlorophyll Maxima
Biogeochemical cycles - NPP and GPP?
Net and Gross Primary Production
Biogeochemical cycles - u and umax (micro)?
Phytoplankton growth rate
What are the major elements (as ions) in the oceans?
Top 6 major elements as ions in the sea (make 99% of dissolved salts). Cl-, Na+, Mg2+, SO42-, Ca2+, K+. Mainly conserved and present in ~constant proportions throughout oceans. But these are not limiting nutrients.
What are MACRONUTRIENTS/ELEMENTS important for plankton?
C, H, O, N, P, S, Mg, K, Ca, Si. Those in bold are in low concentrations umol/kg and can be limiting nutrients to phytoplankton.
What are MICRONUTRIENTS/ELEMENTS important for plankton?
Fe, Mn, Cu, Zn, Mo, Cd, V, Co
What was Iron enrichment experiment?
Large areas of open ocean & equatorial South Pacific respond. Natural iron fertilisation events in the post glacial periods suggest up to 60 billion tons carbon drawn out of the atmosphere, dropping global temps. Lab experiments - 1 ton Fe -> 30 - 100k tons C out of atmosphere. Small-scale experiments - can draw some C out, less efficiently and less permanently (up to 1000 tons per Fe).
What is the microbial food web?
A lot of phytoplankton biomass is predated by grazing: micro and mesozooplankton. Aggregates from senescent biomass and fecal pellets sinks. Some of this is decomposed (respired, releasing CO2) by bacteria, some sinks to ocean floor sequestering the carbon. However, misses viruses, volatile gases and the importance of different macro- and micro- nutrients in driving the microbial system to maintain life in the oceans. DMS - dimethyl sulfide. Volatile gas found in surface water produced by enzymatic lyses of DMSP dimethylsulfoniopropionate by microalgae, atmosphere it is primary component of cloud condensation nuclei.
What are some aggregates?
Faecal pellets from zooplankton, senescent biomass, sink to the depths, marine snow, exports nutrients, depletes surface
How much Carbon is in major reservoirs on earth?
Atmosphere 720 Gt, Oceans 38,400 Gt, Terrestrial biosphere (total) - mainly forests 2,000 Gt. Over the past 200 years, human activities have altered the global carbon cycle significantly. Approx. 30-4-% of the CO2 from human activity released into the atmosphere dissolves into oceans, rivers and lakes.
What happens in the Ocean Carbon Cycle?
POC and DOC, of the anthropogenic CO2 released into the atmosphere some is taken up by the ocean. Some CO2 returns to the atmosphere, and some is exported to the deep ocean. In figure (page 13) CO2 is pumped in, sink into the sediment and deep ocean. A biological pump, in this we have microbial food we have cycling of particulate carbon, eaten by zooplankton and bacteria -> DPC and respired by bacteria into the atmosphere. Very large area of research, what constitutes these and how they are cycled is still an active area.
What happens in the Biological Carbon Pump?
Calcification Inorganic carbon. Phyto capturing CO2, dissolves and reacts with water to produce glucose via photosynthesis. Nutrients come through run off from land or upwelling from the deep. When the nutrients, light and CO2 come together, you create phytoplankton biomass that feeds into the food webs in the oceans. Another component of carbon cycling - carbonate. Weathering of rock releases Ca, which then combines with carbonate to produce calcium carbonate. Some of these calcareous organisms then sink into the sediment. You would think this captures carbon, however due to bacterial respiration this isn’t necessarily so - different areas of the ocean may provide different results depending on local conditions.
What is formanifera?
Scanning electron micrograph of the foramiferan Elphidium gunteri, 1931 ‘test’. Tests or shells are made of calcium carbonate. Sink to ocean floor and fossilise, incorporated into stone. Single-celled organisms.
What is the difference between Formanifera and other seashells?
Formanifera, is a protozoan, the rest are animals. Same protective strategy/buoyancy control. Convergent evolution.
How are classifications dynamic?
Today protista are not treated as a formal taxon but the term ‘protist’ is still commonly used for convenience. The most popular contemporary definition is a phylogenetic one, catch all where a protist is any eukaryote that is not an animals, (land) plant, or (true) fungus.
What is the formaniferan structure?
Endoplasm, ectoplasm, chamber, pores, foramen, food vacuole, nucleus, mitochondria, granureticulose, pseudopodia, granules, primary aperature, food particle, golgi apparatus, ribosomes.