Nitrogen and carbon isotopic ratios of chlorophyll from marine phytoplankton

The relationship between the nitrogen and carbon isotopic ratios of chlorop hyll a and total biomass was explored in cultured marine phytoplankton to a ssess the utility of chlorophyll as an isotopic proxy for photoautotrophs. A near constant nitrogen isotopic depletion of 5.06 +/- 1.13 parts per thou sand (95% confidence interval) in chlorophyll a relative to total nitrogen was observed in 8 species. This value was similar to isotopic differences b etween chlorophyll a and marine particles (5.27 +/- 1.48 parts per thousand (1 sigma); n = 6) and sediments (5.39 +/- 0.67 parts per thousand (1 sigma ); n = 4) in a variety of settings. These findings suggest that a 5.1 parts per thousand isotopic depletion of chlorophyll a relative to total algal n itrogen is a robust relationship that justifies the use of chlorophyll as a nitrogen isotopic surrogate for photoautotrophs. Although interspecies dif ferences in Delta delta(15)N(cell-Chla) exist, and growth rate has a small effect on this parameter, the field data suggest these factors are probably minimized in the ocean where multiple species and growth rates occur. The nitrogen isotopic depletion of chlorophyll a probably occurs during the tra nsamination of glutamic acid in delta-aminolevulinic acid biosynthesis, the first committed precursor to chlorophyll. The carbon isotopic composition of chlorophyll from 12 batch cultures and 7 species of marine phytoplankton was elevated by 0.32 +/- 1.61 parts per th ousand (95% confidence interval) relative to total cellular carbon. No sign ificant interspecies variance was observed that was not attributable to int raspecies variance. There was a moderate inverse correlation between growth rate and Delta delta(13)C(cell-Chla), and it is hypothesized that this par ameter is largely responsible for the large range of intraspecies Delta del ta(13)C(cell-Chla) values observed in batch cultures. Copyright (C) 1999 El sevier Science Ltd.