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  • 1
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 1998-07-10
    Description: Next to N2 gas, the largest pool of reduced nitrogen in the ocean resides in the enormous reservoir of dissolved organic nitrogen (DON). The chemical identity of most of this material, and the mechanisms by which it is cycled, remain fundamental questions in contemporary oceanography. Amino acid enantiomeric ratios in the high molecular weight fraction of DON from surface and deep water in three ocean basins show substantial enrichment in D enantiomers of four amino acids. The magnitude and pattern of these D/L enrichments indicate that peptidoglycan remnants derived from bacterial cell walls constitute a major source of DON throughout the sea. These observations suggest that structural properties of specific bacterial biopolymers, and the mechanisms for their accumulation, are among the central controls on long-term cycling of dissolved organic nitrogen in the sea.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉McCarthy -- Hedges -- Benner -- New York, N.Y. -- Science. 1998 Jul 10;281(5374):231-4.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉M. D. McCarthy and J. I. Hedges, University of Washington, School of Oceanography, Box 357940, Seattle, WA 98195, USA. R. Benner, University of Texas, Marine Science Institute, Port Aransas, TX 78373, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/9657711" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2013-12-18
    Description: The North Pacific subtropical gyre (NPSG) plays a major part in the export of carbon and other nutrients to the deep ocean. Primary production in the NPSG has increased in recent decades despite a reduction in nutrient supply to surface waters. It is thought that this apparent paradox can be explained by a shift in plankton community structure from mostly eukaryotes to mostly nitrogen-fixing prokaryotes. It remains uncertain, however, whether the plankton community domain shift can be linked to cyclical climate variability or a long-term global warming trend. Here we analyse records of bulk and amino-acid-specific (15)N/(14)N isotopic ratios (delta(15)N) preserved in the skeletons of long-lived deep-sea proteinaceous corals collected from the Hawaiian archipelago; these isotopic records serve as a proxy for the source of nitrogen-supported export production through time. We find that the recent increase in nitrogen fixation is the continuation of a much larger, centennial-scale trend. After a millennium of relatively minor fluctuation, delta(15)N decreases between 1850 and the present. The total shift in delta(15)N of -2 per mil over this period is comparable to the total change in global mean sedimentary delta(15)N across the Pleistocene-Holocene transition, but it is happening an order of magnitude faster. We use a steady-state model and find that the isotopic mass balance between nitrate and nitrogen fixation implies a 17 to 27 per cent increase in nitrogen fixation over this time period. A comparison with independent records suggests that the increase in nitrogen fixation might be linked to Northern Hemisphere climate change since the end of the Little Ice Age.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Sherwood, Owen A -- Guilderson, Thomas P -- Batista, Fabian C -- Schiff, John T -- McCarthy, Matthew D -- England -- Nature. 2014 Jan 2;505(7481):78-81. doi: 10.1038/nature12784. Epub 2013 Dec 15.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉1] Ocean Sciences Department, University of California, Santa Cruz, California 95064, USA [2] Institute of Arctic and Alpine Research, University of Colorado, Boulder, Colorado 80309, USA. ; 1] Ocean Sciences Department, University of California, Santa Cruz, California 95064, USA [2] Lawrence Livermore National Laboratory, Livermore, California 94550, USA [3] Institute for Marine Sciences, University of California, Santa Cruz, California 95064, USA. ; Ocean Sciences Department, University of California, Santa Cruz, California 95064, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24336216" target="_blank"〉PubMed〈/a〉
    Keywords: Amino Acids/chemistry ; Animals ; Anthozoa/chemistry/metabolism ; Aquatic Organisms/*metabolism ; Climate Change ; Ecosystem ; Hawaii ; History, 15th Century ; History, 16th Century ; History, 17th Century ; History, 19th Century ; History, 20th Century ; History, 21st Century ; History, Ancient ; History, Medieval ; *Ice Cover ; Nitrates/analysis ; *Nitrogen Fixation ; Nitrogen Isotopes/analysis ; Pacific Ocean ; Plankton/metabolism ; Radiometric Dating ; Seawater/chemistry ; Time Factors ; Tropical Climate
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2015-11-28
    Description: Climate change is predicted to alter marine phytoplankton communities and affect productivity, biogeochemistry, and the efficacy of the biological pump. We reconstructed high-resolution records of changing plankton community composition in the North Pacific Ocean over the past millennium. Amino acid-specific delta(13)C records preserved in long-lived deep-sea corals revealed three major plankton regimes corresponding to Northern Hemisphere climate periods. Non-dinitrogen-fixing cyanobacteria dominated during the Medieval Climate Anomaly (950-1250 Common Era) before giving way to a new regime in which eukaryotic microalgae contributed nearly half of all export production during the Little Ice Age (~1400-1850 Common Era). The third regime, unprecedented in the past millennium, began in the industrial era and is characterized by increasing production by dinitrogen-fixing cyanobacteria. This picoplankton community shift may provide a negative feedback to rising atmospheric carbon dioxide concentrations.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉McMahon, Kelton W -- McCarthy, Matthew D -- Sherwood, Owen A -- Larsen, Thomas -- Guilderson, Thomas P -- New York, N.Y. -- Science. 2015 Dec 18;350(6267):1530-3. doi: 10.1126/science.aaa9942. Epub 2015 Nov 26.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Ocean Sciences, University of California-Santa Cruz, Santa Cruz, CA 95064, USA. Institute for Marine Sciences, University of California-Santa Cruz, Santa Cruz, CA 95064, USA. ; Department of Ocean Sciences, University of California-Santa Cruz, Santa Cruz, CA 95064, USA. ; Institute of Arctic and Alpine Research, University of Colorado-Boulder, Boulder, CO 80309, USA. ; Leibniz Laboratory for Radiometric Dating and Stable Isotope Research, Christian-Albrechts-Universitat zu Kiel, 24118 Kiel, Germany. ; Department of Ocean Sciences, University of California-Santa Cruz, Santa Cruz, CA 95064, USA. Institute for Marine Sciences, University of California-Santa Cruz, Santa Cruz, CA 95064, USA. Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26612834" target="_blank"〉PubMed〈/a〉
    Keywords: Amino Acids/chemistry ; Animals ; Anthozoa/chemistry/*metabolism ; Atmosphere/chemistry ; Carbon/metabolism ; Carbon Cycle ; Carbon Dioxide/analysis/*metabolism ; Carbon Isotopes/analysis ; *Climate Change ; Cyanobacteria/chemistry/classification/*metabolism ; Microalgae/classification/*metabolism ; Pacific Ocean ; Seawater
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2016-10-04
    Description: Marine dissolved organic carbon (DOC) is a major global carbon reservoir, yet its cycling remains poorly understood. Previous work suggests DOC molecular size and chemical composition can significantly affect is bioavailability. Thus, DOC size and composition may control DOC cycling and radiocarbon age (via Δ 14 C). Here we show DOC molecular size is correlated to DOC Δ 14 C in the Pacific Ocean. Our results, based on a series of increasing molecular size fractions from three depths in the Pacific, show increasing DOC Δ 14 C with increasing molecular size. We use a size-age distribution model to predict the DOC and Δ 14 C of ultrafiltered DOC. The model predicts both large and small surface DOC with high Δ 14 C, and a narrow range (200-500 Da) of low Δ 14 C DOC. Deep model offsets suggest different size distributions and/or Δ 14 C sources at 670-915 m. Our results suggest molecular size and composition are linked to DOC reactivity and storage in the ocean.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 5
    Publication Date: 2011-01-03
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 6
    Publication Date: 2011-01-19
    Description: Despite the importance of the nitrogen (N) cycle on marine productivity, little is known about variability in N sources and cycling in the ocean in relation to natural and anthropogenic climate change. Beyond the last few decades of scientific observation, knowledge depends largely on proxy records derived from nitrogen stable isotopes (δ15N) preserved in sediments and other bioarchives. Traditional bulk δ15N measurements, however, represent the combined influence of N source and subsequent trophic transfers, often confounding environmental interpretation. Recently, compound-specific analysis of individual amino acids (δ15N-AA) has been shown as a means to deconvolve trophic level versus N source effects on the δ15N variability of bulk organic matter. Here, we demonstrate the first use of δ15N-AA in a paleoceanographic study, through analysis of annually secreted growth rings preserved in the organic endoskeletons of deep-sea gorgonian corals. In the Northwest Atlantic off Nova Scotia, coral δ15N is correlated with increasing presence of subtropical versus subpolar slope waters over the twentieth century. By using the new δ15N-AA approach to control for variable trophic processing, we are able to interpret coral bulk δ15N values as a proxy for nitrate source and, hence, slope water source partitioning. We conclude that the persistence of the warm, nutrient-rich regime since the early 1970s is largely unique in the context of the last approximately 1,800 yr. This evidence suggests that nutrient variability in this region is coordinated with recent changes in global climate and underscores the broad potential of δ15N-AA for paleoceanographic studies of the marine N cycle.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 7
    Publication Date: 2012-01-04
    Description: Author(s): D. Radeck, V. Werner, G. Ilie, N. Cooper, V. Anagnostatou, T. Ahn, L. Bettermann, R. J. Casperson, R. Chevrier, A. Heinz, J. Jolie, D. McCarthy, M. K. Smith, and E. Williams [Phys. Rev. C 85, 014301] Published Tue Jan 03, 2012
    Keywords: Nuclear Structure
    Print ISSN: 0556-2813
    Electronic ISSN: 1089-490X
    Topics: Physics
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  • 8
    Publication Date: 1965-12-01
    Print ISSN: 0006-3444
    Electronic ISSN: 1464-3510
    Topics: Biology , Mathematics , Medicine
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  • 9
    Publication Date: 2013-02-28
    Description: δ15N and δ13C data obtained from samples of proteinaceous deep-sea corals collected from the North Pacific Subtropical Gyre (Hawai'ian archipelago) and the central equatorial Pacific (Line Islands) document multi-decadal to century scale variability in the isotopic composition of surface-produced particulate organic matter exported to the deep sea. Comparison of the δ13C data, where Line Island samples are 0.6‰ more positive than the Hawai'ian samples, support the contention that the North Pacific Subtropical Gyre is more efficient than the tropical upwelling system at trapping and/or recycling nutrients within the mixed layer. δ15N values from the Line Island samples are also more positive than those from the central gyre, and within the Hawai'ian samples there is a gradient with more positive δ15N values in samples from the main Hawai'ian Islands versus French Frigate Shoals in the Northwestern Hawai'ian Islands. The gradient in the Hawai'ian samples likely reflects the relative importance of algal acquisition of metabolic N via dissolved seawater nitrate uptake versus nitrogen fixation. The Hawai'ian sample set also exhibits a strong decrease in δ15N values from the mid-Holocene to present. We hypothesize that this decrease is most likely the result of decreasing tradewinds, and possibly a commensurate decrease in entrainment of more positive δ15N-NO3 subthermocline water masses.
    Print ISSN: 1810-6277
    Electronic ISSN: 1810-6285
    Topics: Biology , Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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  • 10
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