1. Dimethyl sulphide (DMS) is produced by bacterial degradation of dimethylsulfoniopropionate (DMSP) which is abundant in marine algae. DMS is associated with the aerosol formation which influences the global weather through its negative forcing.
DMSP is an organo-sulphur compound common in marine phytoplankton, seaweeds and other aquatic plant species. It is degraded by bacterial action to form 2 volatile compounds one of which is DMS.
2. The increased concentration of MSA is totally in sync with a more efficient ocean biological pump during Ice ages. With Ice age in progress, ocean water was cooled. Hence their carbon dioxide holding capacity increased phenomenally. With more carbon dioxide stored I the water, marine phytoplankton proliferated leading to the increased production of DMSP. DMSP was later degraded to form DMS which was further oxidised to produce MSA.
Concluding, with increased efficiency of biological pump (increased carbon sequestration in the oceans) MSA concentration increased in the oceanic water (mostly polar regions).
3. (B) Due to Thermohaline circulation similar to the oceanic conveyor belt, Atlantic Ocean loses deep water to the Pacific Ocean and receives surface water from central and south Atlantic as well as water from Greenland. This surface water is relatively poor in nutrients, while the deep waters sent to pacific is high in the nutrient. This leads to a low nutrient in Atlantic and high nutrients in the Pacific.
Moreover, the young Atlantic water has plenty of oxygen while the oxygen content in old pacific water is low since the oxygen has been used up for oxidation and decay purpose.
27) (6 pts) We saw in class (and in the plot below, from class) that when...