Preserved particulate organic carbon is likely derived from the subsurface sulfidic photic zone of the Proterozoic Ocean: evidence from a modern, oxygen-deficient lake.

Autor: Cohen AB; School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, New York, USA., Christensen LN; Cold Spring Harbor Laboratory, Cold Spring Harbor, New York, USA., Weber F; Alfred-Wegener-Institut Helmholtz-Zentrum für Polar und Meeresforschung, Biologische Anstalt Helgoland, Helgoland, Germany., Yagudaeva M; School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, New York, USA., Lo E; School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, New York, USA., Henkes GA; School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, New York, USA.; Department of Geosciences, Stony Brook University, Stony Brook, New York, USA., McCormick ML; Biology Department, Hamilton College, Clinton, New York, USA., Taylor GT; School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, New York, USA.
Jazyk: angličtina
Zdroj: Geobiology [Geobiology] 2024 Mar-Apr; Vol. 22 (2), pp. e12593.
DOI: 10.1111/gbi.12593
Abstrakt: Biological processes in the Proterozoic Ocean are often inferred from modern oxygen-deficient environments (MODEs) or from stable isotopes in preserved sediment. To date, few MODE studies have simultaneously quantified carbon fixation genes and attendant stable isotopic signatures. Consequently, how carbon isotope patterns reflect these pathways has not been thoroughly vetted. Addressing this, we profiled planktonic productivity and quantified carbon fixation pathway genes and associated organic carbon isotope values (δ 13 C POC ) of size-fractionated (0.2-2.7 and >2.7 μm) particulate matter from meromictic Fayetteville Green Lake, NY, USA. The high-O 2 Calvin-Benson-Bassham (CBB) gene (cbbL) was most abundant in the <2.7 μm size fraction in shallow oxic and deep hypoxic waters, corresponding with cyanobacterial and eukaryote algal populations. The low-O 2 CBB gene (cbbM) was most abundant near the lower oxycline boundary in the larger size fraction, coincident with purple sulfur bacteria populations. The reverse citric acid cycle gene (aclB) was equally abundant in both size fractions in the deepest photic zone, coinciding with green sulfur bacteria populations. Methane coenzyme reductase A (mcrA), of anaerobic methane cyclers, was most abundant at the lower oxycline boundary in both size fractions, coinciding with Methanoregula populations. δ 13 C POC values overlapped with the high-O 2 CBB fixation range except for two negative excursions near the lower oxycline boundary, likely reflecting assimilation of isotopically-depleted groundwater-derived carbon by autotrophs and sulfate-reducers. Throughout aphotic waters, δ 13 C POC values of the large size fraction became 13 C-enriched, likely reflecting abundant purple sulfur bacterial aggregates. Eukaryote algae- or cyanobacteria-like isotopic signatures corresponded with increases in cbbL, cbbM, and aclB, and enrichment of exopolymer-rich prokaryotic photoautotrophs aggregates. Results suggest that δ 13 C POC values of preserved sediments from areas of the Proterozoic Ocean with sulfidic photic zones may reflect a mixture of alternate carbon-fixing populations exported from the deep photic zone, challenging the paradigm that sedimentary stable carbon isotope values predominantly reflect oxygenic photosynthesis from surface waters.
(© 2024 John Wiley & Sons Ltd.)
Databáze: MEDLINE
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