期刊
LIMNOLOGY AND OCEANOGRAPHY
卷 56, 期 4, 页码 1489-1503出版社
WILEY
DOI: 10.4319/lo.2011.56.4.1489
关键词
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资金
- National Science Foundation [0080381, 0621014, 0542645, 0542635, EAR-0524778]
- European Association of Organic Geochemists
- Environmental Protection Agency (EPA) [FP916722010]
- Netherlands Organization for Scientific Research [833.02.2002]
- Darwin Center for Biogeology [142.16.1052]
- Direct For Biological Sciences
- Division Of Environmental Biology [0542645, 0621014, 0542635, 0080381] Funding Source: National Science Foundation
- Division Of Environmental Biology
- Direct For Biological Sciences [1042551] Funding Source: National Science Foundation
We tracked carbon (C) and nitrogen (N) uptake into sediments in the presence and absence of benthic macroalgae using dual stable isotope tracers in combination with compound-specific isotope analyses of hydrolyzable amino acids and phospholipid-linked fatty acids to quantify the uptake and retention of C and N within bulk sediments, benthic microalgae (BMA), and heterotrophic bacteria. Stable isotope tracers (as (NH4+)-N-15 and (HCO3-)-C-13) were added to mesocosms either via the surface water or pore water for the first 14 d of the 42-d experiment. Macroalgae and sediments exposed to ambient light and dark cycles rapidly took up label from both sources and retained label for at least 4 weeks after isotope additions ended. BMA dominated sediment uptake of C-13 and N-15, initially accounting for 100% of total uptake. Over time, heterotrophic bacterial uptake became relatively more important, increasing from 0% on day 1 to 20-50% on day 42, indicating a close coupling between BMA and bacterial production. In treatments with macroalgae, sediment C-13 and N-15 uptake was similar to 40% lower than treatments without macroalgae, likely because of shading of the sediment surface by macroalgae, which decreased BMA production, which in turn decreased bacterial production. Overall, sediments served as a sink for C and N through uptake and retention by the microbial community, but retention was lower in the presence of macroalgae.
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