Pigment alterations in the brown mussel Perna perna.

Potential sex and/or gametogenic stage differences in the metabolism of chlorophyll-a and carotenoids in the brown mussel Perna perna of southern Brazil were studied using high performance liquid chromatography (HPLC). Carotenoids derived directly from diet (phytoplankton) were fucoxanthin plus diatoxanthin (diatoms), alloxanthin (cryptophytes) and zeaxanthin (mainly cyanobacteria). Females accumulated carotenoid-diols and epoxides (~3-4 mg/g-dry wt.) while males had much lower concentrations (~0.7 mg/g-dry wt.). An antioxidant/free radical scavenging role is proposed for carotenoids in females. Mean ratios of chlorophyll plus derivatives (Chlns-a) to carotenoids for male and female P. perna were 50:1 and 4:1, respectively. The higher ratio in males relates to both higher carotenoid contents in females plus higher total Chlns-a in males (~22 mg/g-dry wt.), relative to the females (~4 mg/g-dry wt.). Chlorophyll-a metabolism in both sexes followed two distinct pathways. First, cyclization of pyropheophorbide-a gave 13(2), 17(3)-cyclopheophorbide-a-enol (CPPaE) which was further oxidized to hydroxy-chlorophyllone. Second, chlorophyll-a derivatives retaining the 13(2)-carbomethoxy moiety were oxidized to purpurin-18 which was hydrolyzed to chlorin-p(6). In both cases, metabolism of dietary chlorophyll-a was oxidative and derivatives could either serve as antioxidants or merely be the results of non-specific digestive processes.

The post-Paleozoic chronology and mechanism of 13C depletion in primary marine organic matter.

Carbon-isotopic compositions of geoporphyrins have been measured from marine sediments of Mesozoic and Cenozoic age in order to elucidate the timing and extent of depletion of 13C in marine primary producers. These results indicate that the difference in isotopic composition of coeval marine carbonates and marine primary photosynthate was approximately 5 to 7 permil greater during the Mesozoic and early Cenozoic than at present. In contrast to the isotopic record of marine primary producers, isotopic compositions of terrestrial organic materials have remained approximately constant for this same interval of time. This difference in the isotopic records of marine and terrestrial organic matter is considered in terms of the mechanisms controlling the isotopic fractionation associated with photosynthetic fixation of carbon. We show that the decreased isotopic fractionation between marine carbonates and organic matter from the Early to mid-Cenozoic may record variations in the abundance of atmospheric CO2.