Ll. King, A MASS-BALANCE OF CHLOROPHYLL DEGRADATION PRODUCT ACCUMULATION IN BLACK-SEA SEDIMENTS, Deep-sea research. Part 1. Oceanographic research papers, 42(6), 1995, pp. 919-942
The distribution of chlorophyll degradation products was measured in B
lack Sea sediment trap and sediment samples. Chlorophyll degradation p
roducts were identified as free phorbins, phorbin steryl esters, high
molecular weight chlorophyll degradation products, and acid extractabl
e chlorophyll degradation products. When all these sinks are considere
d, an inventory of chlorophyll degradation products can be established
which identifies four times more sedimentary phorbins than standard H
PLC studies alone. The concentration of total chlorophyll degradation
products in the sediment trap samples varies with season and, in the s
ediments, increases with depth from Unit I into Unit II. In Unit III s
ediments, the total phorbin concentration dramatically decreases, Thes
e trends are similar to those of the total organic carbon concentratio
n. Variations in the ratio of total phorbin/total organic carbon with
depth in the sediments appear to be related to previously suggested ch
anges of oxygen concentrations over time in the Black Sea water column
. This new data was combined with data from the literature to create a
mass balance of chlorophyll flux, degradation, and accumulation in th
e Black Sea. It is concluded that once chlorophyll degradation product
s reach the anoxic water column, they survive to be deposited in the u
nderlying sediments. Although a larger percentage of total organic car
bon, compared to total phorbin, passes out of the photic zone, the pho
rbin macrocycle appears to be more stable under anoxic conditions than
is total organic carbon.