Nutrient recycling and the stoichiometric relationship among C, N, and P in Paleozoic anoxic sediments
Abstract
Remineralized organic N and P diffused into the water column from underlying anoxic sediments were important sources of macronutrients for primary production in shallow Paleozoic epicontinental seas. Ratios of total organic C to total N or P in ancient sediments that are greater than Redfield-like values are often cited as evidence for macronutrient recycling. We propose that the stoichiometric relationship among C, N, and P in anoxic Paleozoic sediments was mediated primarily by heterotrophic bacterial alkaline phosphatases. Bacterial heterotrophy in organic-rich anaerobic sediments is frequently limited by the availability of labile (low C/N) organic matter. In response, bacterial heterotrophs invest scarce C and N to produce alkaline phosphatases in order to alleviate labile organic matter limitation by hydrolysis of organophosphates. This suggests that sediment organic C/N may represent a threshold beyond which the investment of intracellular C and N in the production of alkaline phosphatase no longer results in a stoichiometrically favorable return on the investment. If this is the case, then C/P likely represents the point in the diagenesis of organic matter at which the effectiveness of alkaline phosphatase in procuring labile organic matter by remineralization of P is constrained by the lability of the organic matter itself. Because alkaline phosphatase activity is expressed in inverse proportion to the porewater concentration of phosphate, at a given distance from the terrestrial source of weathered P, an equilibrium determined by total phosphate influx results in consistent total P burial rates and consistent organic C/N values independent of the total organic content of the sediment. To account for consistent C/N in spite of variable total organic carbon at a given location, we propose that variations in the absolute abundance of organic C in organic-rich Devonian sediments were largely a function of the lipid content of algal primary producers. The significance of this research is two-fold: First, it puts forth a novel mechanistic explanation for observed relationships among C, N, and P in ancient sediments based upon observations of modern microbial ecosystems. Second, it links the preservation of organic matter in the geological record to the nutritional status of primary producers.
- Publication:
-
AGU Fall Meeting Abstracts
- Pub Date:
- December 2016
- Bibcode:
- 2016AGUFMPP23B2332T
- Keywords:
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- 4845 Nutrients and nutrient cycling;
- OCEANOGRAPHY: BIOLOGICAL AND CHEMICALDE: 4912 Biogeochemical cycles;
- processes;
- and modeling;
- PALEOCEANOGRAPHY