More double-bonds are biosynthesised by coccolithophores at lowertemperatures to maintain membrane fluidity (in alkanones)
alkanone is an aldehyde and and alkene
Gibbs free energy equation is delta G = -RTln K
iron is the fourth most abundant element in the crust - 5%
Rapid reactions thus occurred and resulted in highly reducingconditions in the paleo ocean
Transport from continents occurred as they were formed andhydrological cycle initiated weathering
Early life evolved in environment rich in dissolved Fe
Fe levels and bioavailability are controlled by redox processes
Dust deposition – the major source of Fe to surface ocean• Very low input into Pacific subtropical gyres and Southern OceanMain HNLC regions – Southern Ocean and Equatorial Pacific
the diagenetic sequence is determined by the respective change in the electrode potential in reduction of these compounds - the energy yield is highest with o2 and then decreases downwards