Chapter 25: Flashcards
Carbon cycle
Atmosphere to vegetation to soils, to benthic sediments,
Atmosphere to surface ocean waters, used by marine biota, flux from marine biota to deep ocean waters
- When water cools it drops to deep waters
- Driven by temperature and salinity
Global oceanic pattern
Mass of atmospheric carbon
750Pg (1 Petagram = 10^15g)
Mass of carbon in rocks
60 000 000 Pg
Mass of marine biota carbon
3Pg
5 Pools
Atmosphere Forests and Fauna Soils Deep ocean Rocks and sediment
Percentages of anthropogenic C release
20% deforestation, 80% burning fossil fuels
More CO2 in the air results in shell weakening in organisms (shell are harder to make), decreased calcification of coral reefs
Ocean acidification
Mechanism of ocean acidification
CO2 forms carbonic acid
Ecologist who showos acidified lake produce skinny fucked up looking fish and crayfish
David Schindler