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  • Blackwell Publishing Ltd  (2)
  • John Wiley & Sons  (1)
  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    FEMS microbiology ecology 8 (1991), S. 0 
    ISSN: 1574-6941
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    FEMS microbiology letters 85 (1991), S. 0 
    ISSN: 1574-6968
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Abstract The utilization of glutamic acid and alanine in anoxic marine sediments was studied using sediments collected from a tidal flat on the Atlantic Ocean side of Virginia's Eastern Shore (Bordens-take Bay) and a site in the mid-Chesapeake Bay. At both sites volatile fatty acids (VFAs) were produced as intermediates in the catabolism (or oxidation) of both amino acids. In contrast, methylated amines were not produced as metabolic intermediates from either amino acid. The addition of 20 mM molybdate to sediment slurries (to inhibit bacterial sulfate reduction) led to the continuous production of VFAs from both amino acids, indicating that the majority of this VFA production from these amino acids occurred by fermentative processes. Non-catabolic uptake of these amino acids (presumably into bacterial bio-mass) also appeared to be an important process in removing alanine and glutamic acid from these sediment slurries. A kinetic model used to analyze these data indicated that ? 85% of the alanine catabolism occurred by fermentative processes, with remineralization by sulfate reducing bacteria accounting for the difference. In contrast, all of the glutamic acid catabolism appeared to occur by fermentation. Calculations using data on VFA and ΣCO2 production in molybdate inhibited sediments also suggested that acetate and formate were the predominant VFAs produced by the fermentation of alanine, and perhaps glutamic acid as well. The oxidation of dissolved, free amino acids appeared to account for a significant fraction of the ammonium production in these anoxic marine sediments, although amino acids represented less than ? 2% of the carbon sources/electron donors used by sulfate reduction. These observations suggest that the general pathway of amino acid utilization in anoxic sediments involves their oxidation by fermentative bacteria to produce compounds such as VFA or H2 which are then themselves used as substrates by either sulfate reducing or methanogenic bacteria. As such, dissolved free amino acids appear to play an important role as intermediates in carbon and nitrogen cycling in these environments.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2018. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Global Biogeochemical Cycles 32 (2018): 389-416, doi:10.1002/2017GB005790.
    Description: Carbon cycling in the coastal zone affects global carbon budgets and is critical for understanding the urgent issues of hypoxia, acidification, and tidal wetland loss. However, there are no regional carbon budgets spanning the three main ecosystems in coastal waters: tidal wetlands, estuaries, and shelf waters. Here we construct such a budget for eastern North America using historical data, empirical models, remote sensing algorithms, and process‐based models. Considering the net fluxes of total carbon at the domain boundaries, 59 ± 12% (± 2 standard errors) of the carbon entering is from rivers and 41 ± 12% is from the atmosphere, while 80 ± 9% of the carbon leaving is exported to the open ocean and 20 ± 9% is buried. Net lateral carbon transfers between the three main ecosystem types are comparable to fluxes at the domain boundaries. Each ecosystem type contributes substantially to exchange with the atmosphere, with CO2 uptake split evenly between tidal wetlands and shelf waters, and estuarine CO2 outgassing offsetting half of the uptake. Similarly, burial is about equal in tidal wetlands and shelf waters, while estuaries play a smaller but still substantial role. The importance of tidal wetlands and estuaries in the overall budget is remarkable given that they, respectively, make up only 2.4 and 8.9% of the study domain area. This study shows that coastal carbon budgets should explicitly include tidal wetlands, estuaries, shelf waters, and the linkages between them; ignoring any of them may produce a biased picture of coastal carbon cycling.
    Description: NASA Interdisciplinary Science program Grant Number: NNX14AF93G; NASA Carbon Cycle Science Program Grant Number: NNX14AM37G; NASA Ocean Biology and Biogeochemistry Program Grant Number: NNX11AD47G; National Science Foundation's Chemical Oceanography Program Grant Number: OCE‐1260574
    Description: 2018-10-04
    Keywords: Carbon cycle ; Coastal zone ; Tidal wetlands ; Estuaries ; Shelf waters
    Repository Name: Woods Hole Open Access Server
    Type: Article
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