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  • Nature Publishing Group (NPG)  (121)
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  • 1
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    The trophic fingerprint of marine fisheries (2010)
    Nature Publishing Group (NPG)
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    Publication Date: 2010-11-19
    Description: Biodiversity indicators provide a vital window on the state of the planet, guiding policy development and management. The most widely adopted marine indicator is mean trophic level (MTL) from catches, intended to detect shifts from high-trophic-level predators to low-trophic-level invertebrates and plankton-feeders. This indicator underpins reported trends in human impacts, declining when predators collapse ("fishing down marine food webs") and when low-trophic-level fisheries expand ("fishing through marine food webs"). The assumption is that catch MTL measures changes in ecosystem MTL and biodiversity. Here we combine model predictions with global assessments of MTL from catches, trawl surveys and fisheries stock assessments and find that catch MTL does not reliably predict changes in marine ecosystems. Instead, catch MTL trends often diverge from ecosystem MTL trends obtained from surveys and assessments. In contrast to previous findings of rapid declines in catch MTL, we observe recent increases in catch, survey and assessment MTL. However, catches from most trophic levels are rising, which can intensify fishery collapses even when MTL trends are stable or increasing. To detect fishing impacts on marine biodiversity, we recommend greater efforts to measure true abundance trends for marine species, especially those most vulnerable to fishing.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Branch, Trevor A -- Watson, Reg -- Fulton, Elizabeth A -- Jennings, Simon -- McGilliard, Carey R -- Pablico, Grace T -- Ricard, Daniel -- Tracey, Sean R -- England -- Nature. 2010 Nov 18;468(7322):431-5. doi: 10.1038/nature09528.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉School of Aquatic and Fishery Sciences, Box 355020, University of Washington, Seattle, Washington 98195-5020, USA. tbranch@uw.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21085178" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Aquatic Organisms/*isolation & purification/*metabolism ; Biodiversity ; Biomass ; Databases, Factual ; *Ecosystem ; Environmental Policy ; *Fisheries ; *Fishes/metabolism ; Food Chain ; Human Activities ; Invertebrates/metabolism ; Models, Biological ; Plankton/metabolism
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 2
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    Negative plant-soil feedback predicts tree-species relative abundance in a tropical forest (2010)
    Nature Publishing Group (NPG)
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    Publication Date: 2010-06-29
    Description: The accumulation of species-specific enemies around adults is hypothesized to maintain plant diversity by limiting the recruitment of conspecific seedlings relative to heterospecific seedlings. Although previous studies in forested ecosystems have documented patterns consistent with the process of negative feedback, these studies are unable to address which classes of enemies (for example, pathogens, invertebrates, mammals) exhibit species-specific effects strong enough to generate negative feedback, and whether negative feedback at the level of the individual tree is sufficient to influence community-wide forest composition. Here we use fully reciprocal shade-house and field experiments to test whether the performance of conspecific tree seedlings (relative to heterospecific seedlings) is reduced when grown in the presence of enemies associated with adult trees. Both experiments provide strong evidence for negative plant-soil feedback mediated by soil biota. In contrast, above-ground enemies (mammals, foliar herbivores and foliar pathogens) contributed little to negative feedback observed in the field. In both experiments, we found that tree species that showed stronger negative feedback were less common as adults in the forest community, indicating that susceptibility to soil biota may determine species relative abundance in these tropical forests. Finally, our simulation models confirm that the strength of local negative feedback that we measured is sufficient to produce the observed community-wide patterns in tree-species relative abundance. Our findings indicate that plant-soil feedback is an important mechanism that can maintain species diversity and explain patterns of tree-species relative abundance in tropical forests.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Mangan, Scott A -- Schnitzer, Stefan A -- Herre, Edward A -- Mack, Keenan M L -- Valencia, Mariana C -- Sanchez, Evelyn I -- Bever, James D -- R01 GM092660/GM/NIGMS NIH HHS/ -- England -- Nature. 2010 Aug 5;466(7307):752-5. doi: 10.1038/nature09273.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Biological Sciences, University of Wisconsin-Milwaukee, Wisconsin 53201, USA. smangan37@gmail.com〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20581819" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; *Biodiversity ; Biomass ; Computer Simulation ; Feedback, Physiological ; Food Chain ; Insects/physiology ; Models, Biological ; Panama ; Population Density ; Seedlings/growth & development ; Soil/*analysis ; *Soil Microbiology ; Species Specificity ; Trees/*classification/*growth & development/microbiology/parasitology ; *Tropical Climate ; Vertebrates/physiology
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 3
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    Loss of plant species after chronic low-level nitrogen deposition to prairie grasslands (2008)
    Nature Publishing Group (NPG)
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    Publication Date: 2008-02-08
    Description: Rates of atmospheric deposition of biologically active nitrogen (N) are two to seven times the pre-industrial rates in many developed nations because of combustion of fossil fuels and agricultural fertilization. They are expected to increase similarly over the next 50 years in industrializing nations of Asia and South America. Although the environmental impacts of high rates of nitrogen addition have been well studied, this is not so for the lower, chronic rates that characterize much of the globe. Here we present results of the first multi-decadal experiment to examine the impacts of chronic, experimental nitrogen addition as low as 10 kg N ha(-1) yr(-1) above ambient atmospheric nitrogen deposition (6 kg N ha(-1) yr(-1) at our site). This total input rate is comparable to terrestrial nitrogen deposition in many industrialized nations. We found that this chronic low-level nitrogen addition rate reduced plant species numbers by 17% relative to controls receiving ambient N deposition. Moreover, species numbers were reduced more per unit of added nitrogen at lower addition rates, suggesting that chronic but low-level nitrogen deposition may have a greater impact on diversity than previously thought. A second experiment showed that a decade after cessation of nitrogen addition, relative plant species number, although not species abundances, had recovered, demonstrating that some effects of nitrogen addition are reversible.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Clark, Christopher M -- Tilman, David -- England -- Nature. 2008 Feb 7;451(7179):712-5. doi: 10.1038/nature06503.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Ecology, Evolution and Behavior, 100 Ecology, 1987 Upper Buford Circle, University of Minnesota, St. Paul, Minnesota 55108, USA. clark134@umn.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18256670" target="_blank"〉PubMed〈/a〉
    Keywords: *Biodiversity ; Biomass ; *Ecosystem ; Nitrogen/*metabolism ; Plants/classification/*metabolism ; *Poaceae/metabolism ; Random Allocation ; Time Factors
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 4
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    Net carbon dioxide losses of northern ecosystems in response to autumn warming (2008)
    Nature Publishing Group (NPG)
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    Publication Date: 2008-01-04
    Description: The carbon balance of terrestrial ecosystems is particularly sensitive to climatic changes in autumn and spring, with spring and autumn temperatures over northern latitudes having risen by about 1.1 degrees C and 0.8 degrees C, respectively, over the past two decades. A simultaneous greening trend has also been observed, characterized by a longer growing season and greater photosynthetic activity. These observations have led to speculation that spring and autumn warming could enhance carbon sequestration and extend the period of net carbon uptake in the future. Here we analyse interannual variations in atmospheric carbon dioxide concentration data and ecosystem carbon dioxide fluxes. We find that atmospheric records from the past 20 years show a trend towards an earlier autumn-to-winter carbon dioxide build-up, suggesting a shorter net carbon uptake period. This trend cannot be explained by changes in atmospheric transport alone and, together with the ecosystem flux data, suggest increasing carbon losses in autumn. We use a process-based terrestrial biosphere model and satellite vegetation greenness index observations to investigate further the observed seasonal response of northern ecosystems to autumnal warming. We find that both photosynthesis and respiration increase during autumn warming, but the increase in respiration is greater. In contrast, warming increases photosynthesis more than respiration in spring. Our simulations and observations indicate that northern terrestrial ecosystems may currently lose carbon dioxide in response to autumn warming, with a sensitivity of about 0.2 PgC degrees C(-1), offsetting 90% of the increased carbon dioxide uptake during spring. If future autumn warming occurs at a faster rate than in spring, the ability of northern ecosystems to sequester carbon may be diminished earlier than previously suggested.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Piao, Shilong -- Ciais, Philippe -- Friedlingstein, Pierre -- Peylin, Philippe -- Reichstein, Markus -- Luyssaert, Sebastiaan -- Margolis, Hank -- Fang, Jingyun -- Barr, Alan -- Chen, Anping -- Grelle, Achim -- Hollinger, David Y -- Laurila, Tuomas -- Lindroth, Anders -- Richardson, Andrew D -- Vesala, Timo -- England -- Nature. 2008 Jan 3;451(7174):49-52. doi: 10.1038/nature06444.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉LSCE, UMR CEA-CNRS, Batiment 709, CE, L'Orme des Merisiers, F-91191 Gif-sur-Yvette, France. slpiao@lsce.ipsl.fr〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18172494" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/chemistry ; Biomass ; Carbon Dioxide/analysis/*metabolism ; Cell Respiration ; *Ecosystem ; Fossil Fuels ; Geography ; Greenhouse Effect ; History, 20th Century ; History, 21st Century ; Oceans and Seas ; Photosynthesis ; Plant Transpiration ; Plants/metabolism ; Rain ; *Seasons ; Soil/analysis ; *Temperature ; Water/metabolism
    Print ISSN: 0028-0836
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    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 5
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    Old-growth forests as global carbon sinks (2008)
    Nature Publishing Group (NPG)
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    Publication Date: 2008-09-12
    Description: Old-growth forests remove carbon dioxide from the atmosphere at rates that vary with climate and nitrogen deposition. The sequestered carbon dioxide is stored in live woody tissues and slowly decomposing organic matter in litter and soil. Old-growth forests therefore serve as a global carbon dioxide sink, but they are not protected by international treaties, because it is generally thought that ageing forests cease to accumulate carbon. Here we report a search of literature and databases for forest carbon-flux estimates. We find that in forests between 15 and 800 years of age, net ecosystem productivity (the net carbon balance of the forest including soils) is usually positive. Our results demonstrate that old-growth forests can continue to accumulate carbon, contrary to the long-standing view that they are carbon neutral. Over 30 per cent of the global forest area is unmanaged primary forest, and this area contains the remaining old-growth forests. Half of the primary forests (6 x 10(8) hectares) are located in the boreal and temperate regions of the Northern Hemisphere. On the basis of our analysis, these forests alone sequester about 1.3 +/- 0.5 gigatonnes of carbon per year. Thus, our findings suggest that 15 per cent of the global forest area, which is currently not considered when offsetting increasing atmospheric carbon dioxide concentrations, provides at least 10 per cent of the global net ecosystem productivity. Old-growth forests accumulate carbon for centuries and contain large quantities of it. We expect, however, that much of this carbon, even soil carbon, will move back to the atmosphere if these forests are disturbed.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Luyssaert, Sebastiaan -- Schulze, E-Detlef -- Borner, Annett -- Knohl, Alexander -- Hessenmoller, Dominik -- Law, Beverly E -- Ciais, Philippe -- Grace, John -- England -- Nature. 2008 Sep 11;455(7210):213-5. doi: 10.1038/nature07276.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Biology, University of Antwerp, 2610 Wilrijk, Belgium. sebastiaan.luyssaert@ua.ac.be〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18784722" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Atmosphere/chemistry ; Biomass ; Carbon/*metabolism ; Carbon Dioxide/metabolism ; Databases, Factual ; Disasters ; *Ecosystem ; History, 15th Century ; History, 16th Century ; History, 17th Century ; History, 18th Century ; History, 19th Century ; History, 20th Century ; History, 21st Century ; History, Ancient ; History, Medieval ; Human Activities ; Time Factors ; Trees/*metabolism
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 6
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    Imaging in the era of molecular oncology (2008)
    Nature Publishing Group (NPG)
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    Publication Date: 2008-04-04
    Description: New technologies for imaging molecules, particularly optical technologies, are increasingly being used to understand the complexity, diversity and in vivo behaviour of cancers. 'Omic' approaches are providing comprehensive 'snapshots' of biological indicators, or biomarkers, of cancer, but imaging can take this information a step further, showing the activity of these markers in vivo and how their location changes over time. Advances in experimental and clinical imaging are likely to improve how cancer is understood at a systems level and, ultimately, should enable doctors not only to locate tumours but also to assess the activity of the biological processes within these tumours and to provide 'on the spot' treatment.〈br /〉〈br /〉〈a href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC2708079/" target="_blank"〉〈img src="https://static.pubmed.gov/portal/portal3rc.fcgi/4089621/img/3977009" border="0"〉〈/a〉   〈a href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC2708079/" target="_blank"〉This paper as free author manuscript - peer-reviewed and accepted for publication〈/a〉〈br /〉〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Weissleder, Ralph -- Pittet, Mikael J -- P01 CA069246/CA/NCI NIH HHS/ -- P01 CA069246-070006/CA/NCI NIH HHS/ -- P50 CA086355/CA/NCI NIH HHS/ -- P50 CA086355-01/CA/NCI NIH HHS/ -- U24 CA092782/CA/NCI NIH HHS/ -- U24 CA092782-07/CA/NCI NIH HHS/ -- England -- Nature. 2008 Apr 3;452(7187):580-9. doi: 10.1038/nature06917.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Center for Systems Biology, Massachusetts General Hospital, 185 Cambridge Street, CPZN 5206, Boston, Massachusetts 02114, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18385732" target="_blank"〉PubMed〈/a〉
    Keywords: Diagnostic Imaging/methods/*trends ; Fluorescence ; Genes, Reporter ; Humans ; Microscopy ; Molecular Diagnostic Techniques/methods/*trends ; Neoplasms/*diagnosis/genetics/*metabolism/pathology
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  • 7
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    Coherent ecological dynamics induced by large-scale disturbance (2008)
    Nature Publishing Group (NPG)
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    Publication Date: 2008-07-18
    Description: Aggregate community-level response to disturbance is a principle concern in ecology because post-disturbance dynamics are integral to the ability of ecosystems to maintain function in an uncertain world. Community-level responses to disturbance can be arrayed along a spectrum ranging from synchronous oscillations where all species rise and fall together, to compensatory dynamics where total biomass remains relatively constant despite fluctuations in the densities of individual species. An important recent insight is that patterns of synchrony and compensation can vary with the timescale of analysis and that spectral time series methods can enable detection of coherent dynamics that would otherwise be obscured by opposing patterns occurring at different scales. Here I show that application of wavelet analysis to experimentally manipulated plankton communities reveals strong synchrony after disturbance. The result is paradoxical because it is well established that these communities contain both disturbance-sensitive and disturbance-tolerant species leading to compensation within functional groups. Theory predicts that compensatory substitution of functionally equivalent species should stabilize ecological communities, yet I found at the whole-community level a large increase in seasonal biomass variation. Resolution of the paradox hinges on patterns of seasonality among species. The compensatory shift in community composition after disturbance resulted in a loss of cold-season dominants, which before disturbance had served to stabilize biomass throughout the year. Species dominating the disturbed community peaked coherently during the warm season, explaining the observed synchrony and increase in seasonal biomass variation. These results suggest that theory relating compensatory dynamics to ecological stability needs to consider not only complementarity in species responses to environmental change, but also seasonal complementarity among disturbance-tolerant and disturbance-sensitive species.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Keitt, Timothy H -- England -- Nature. 2008 Jul 17;454(7202):331-4. doi: 10.1038/nature06935.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Integrative Biology, University of Texas, Austin, Texas 78712, USA. tkeitt@mail.utexas.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18633416" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Biomass ; Crustacea/physiology ; *Ecosystem ; Fresh Water ; Hot Temperature ; Hydrogen-Ion Concentration ; Plankton/*physiology ; Population Dynamics ; Seasons ; Time Factors
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  • 8
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    Major viral impact on the functioning of benthic deep-sea ecosystems (2008)
    Nature Publishing Group (NPG)
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    Publication Date: 2008-08-30
    Description: Viruses are the most abundant biological organisms of the world's oceans. Viral infections are a substantial source of mortality in a range of organisms-including autotrophic and heterotrophic plankton-but their impact on the deep ocean and benthic biosphere is completely unknown. Here we report that viral production in deep-sea benthic ecosystems worldwide is extremely high, and that viral infections are responsible for the abatement of 80% of prokaryotic heterotrophic production. Virus-induced prokaryotic mortality increases with increasing water depth, and beneath a depth of 1,000 m nearly all of the prokaryotic heterotrophic production is transformed into organic detritus. The viral shunt, releasing on a global scale approximately 0.37-0.63 gigatonnes of carbon per year, is an essential source of labile organic detritus in the deep-sea ecosystems. This process sustains a high prokaryotic biomass and provides an important contribution to prokaryotic metabolism, allowing the system to cope with the severe organic resource limitation of deep-sea ecosystems. Our results indicate that viruses have an important role in global biogeochemical cycles, in deep-sea metabolism and the overall functioning of the largest ecosystem of our biosphere.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Danovaro, Roberto -- Dell'Anno, Antonio -- Corinaldesi, Cinzia -- Magagnini, Mirko -- Noble, Rachel -- Tamburini, Christian -- Weinbauer, Markus -- England -- Nature. 2008 Aug 28;454(7208):1084-7. doi: 10.1038/nature07268.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Marine Science, Faculty of Science, Polytechnic University of Marche, Via Brecce Bianche, 60131 Ancona, Italy. r.danovaro@univpm.it〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18756250" target="_blank"〉PubMed〈/a〉
    Keywords: Biomass ; Carbon/metabolism ; *Ecosystem ; Geologic Sediments/virology ; Heterotrophic Processes ; Hydrostatic Pressure ; Microbial Viability ; Oceans and Seas ; Prokaryotic Cells/cytology/metabolism/virology ; Seawater/*virology ; *Virus Physiological Phenomena ; Viruses/isolation & purification/metabolism
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  • 9
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    Carbon cycle: sources, sinks and seasons (2008)
    Nature Publishing Group (NPG)
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    Publication Date: 2008-01-04
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Miller, John B -- England -- Nature. 2008 Jan 3;451(7174):26-7. doi: 10.1038/451026a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18172488" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/*chemistry ; Biomass ; Carbon Dioxide/analysis/*metabolism ; *Ecosystem ; Fossil Fuels ; Geography ; Greenhouse Effect ; Oceans and Seas ; Plants/metabolism ; *Seasons ; Temperature
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 10
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    Counterintuitive carbon-to-nutrient coupling in an Arctic pelagic ecosystem (2008)
    Nature Publishing Group (NPG)
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    Publication Date: 2008-08-22
    Description: Predicting the ocean's role in the global carbon cycle requires an understanding of the stoichiometric coupling between carbon and growth-limiting elements in biogeochemical processes. A recent addition to such knowledge is that the carbon/nitrogen ratio of inorganic consumption and release of dissolved organic matter may increase in a high-CO(2) world. This will, however, yield a negative feedback on atmospheric CO(2) only if the extra organic material escapes mineralization within the photic zone. Here we show, in the context of an Arctic pelagic ecosystem, how the fate and effects of added degradable organic carbon depend critically on the state of the microbial food web. When bacterial growth rate was limited by mineral nutrients, extra organic carbon accumulated in the system. When bacteria were limited by organic carbon, however, addition of labile dissolved organic carbon reduced phytoplankton biomass and activity and also the rate at which total organic carbon accumulated, explained as the result of stimulated bacterial competition for mineral nutrients. This counterintuitive 'more organic carbon gives less organic carbon' effect was particularly pronounced in diatom-dominated systems where the carbon/mineral nutrient ratio in phytoplankton production was high. Our results highlight how descriptions of present and future states of the oceanic carbon cycle require detailed understanding of the stoichiometric coupling between carbon and growth-limiting mineral nutrients in both autotrophic and heterotrophic processes.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Thingstad, T F -- Bellerby, R G J -- Bratbak, G -- Borsheim, K Y -- Egge, J K -- Heldal, M -- Larsen, A -- Neill, C -- Nejstgaard, J -- Norland, S -- Sandaa, R-A -- Skjoldal, E F -- Tanaka, T -- Thyrhaug, R -- Topper, B -- England -- Nature. 2008 Sep 18;455(7211):387-90. doi: 10.1038/nature07235. Epub 2008 Aug 20.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Biology, University of Bergen, Jahnebakken 5PO Box 7800, 5020 Bergen, Norway. frede.thingstad@bio.uib.no〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18716617" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Arctic Regions ; Atmosphere/chemistry ; Autotrophic Processes/drug effects/radiation effects ; Bacteria/drug effects/growth & development/metabolism/radiation effects ; Biomass ; Carbon/*metabolism ; Carbon Dioxide/metabolism ; Diatoms/metabolism/radiation effects ; *Ecosystem ; Eutrophication ; Food Chain ; Glucose/metabolism/pharmacology ; Heterotrophic Processes/drug effects/radiation effects ; Phytoplankton/drug effects/growth & development/metabolism/radiation effects
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