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how does climate isolate CO2 from atmosphere into ocean
Increased export and production
explain thermohaline circulation
1000 years to make a loop
reduction in deep atlantic circulation during glacial due to cold water
thermohaline circulation proxies
nutrients - isotope 13C DIC distribution atlantic inverse to nutrients
water mass tracers
open circulation proxies
depleted organic material of isotope 13C
during phtosynthesis plants take up lighter 12C isotope leaving organic material depleted in heavier 13C isotope
what proxies show reduction in atlantic ocean ventilation
past SW 13C DIC inferred form of benthic foraminifera
SW 13C DIC has 1:1 ratio with benthic foraminiferal shell 13C
neodymium isotopes (nd) - less in atlantic deep water and more in antarctic bottom water
condition for better preserved organic material
less dissolved O2 in SW