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  • Articles  (19)
  • Wetlands
  • sediment
  • Nature. 452(7189): 864-7. doi: 10.1038/nature06825.  (1)
  • Nature. 453(7193): 383-6. doi: 10.1038/nature06950.  (1)
  • Nature. 454(7203): 515-8. doi: 10.1038/nature06970.  (1)
  • Nature. 455(7217): 1235-9. doi: 10.1038/nature07281.  (1)
  • Nature. 462(7274): 795-8. doi: 10.1038/nature08632.  (1)
  • 328
  • Biology  (19)
  • Energy, Environment Protection, Nuclear Power Engineering
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  • Articles  (19)
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  • 1
    Publication Date: 2009-12-18
    Description: Avian brood parasites and their hosts provide model systems for investigating links between recognition, learning, and their fitness consequences. One major evolutionary puzzle has continued to capture the attention of naturalists for centuries: why do hosts of brood parasites generally fail to recognize parasitic offspring after they have hatched from the egg, even when the host and parasitic chicks differ to almost comic degrees? One prominent theory to explain this pattern proposes that the costs of mistakenly learning to recognize the wrong offspring make recognition maladaptive. Here we show that American coots, Fulica americana, can recognize and reject parasitic chicks in their brood by using learned cues, despite the fact that the hosts and the brood parasites are of the same species. A series of chick cross-fostering experiments confirm that coots use first-hatched chicks in a brood as referents to learn to recognize their own chicks and then discriminate against later-hatched parasitic chicks in the same brood. When experimentally provided with the wrong reference chicks, coots can be induced to discriminate against their own offspring, confirming that the learning errors proposed by theory can exist. However, learning based on hatching order is reliable in naturally parasitized coot nests because host eggs hatch predictably ahead of parasite eggs. Conversely, a lack of reliable information may help to explain why the evolution of chick recognition is not more common in hosts of most interspecific brood parasites.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Shizuka, Daizaburo -- Lyon, Bruce E -- England -- Nature. 2010 Jan 14;463(7278):223-6. doi: 10.1038/nature08655. Epub 2009 Dec 16.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Ecology and Evolutionary Biology, University of California, Santa Cruz, California 95064, USA. shizuka@biology.ucsc.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20016486" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; *Biological Evolution ; Birds/*parasitology/*physiology ; British Columbia ; Cues ; Discrimination Learning/*physiology ; Feeding Behavior/physiology ; Genetic Fitness ; Nesting Behavior/*physiology ; Ovum/growth & development ; Pattern Recognition, Visual/physiology ; Survival Rate ; Time Factors ; Wetlands
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  • 2
    Publication Date: 2008-05-16
    Description: Atmospheric methane is an important greenhouse gas and a sensitive indicator of climate change and millennial-scale temperature variability. Its concentrations over the past 650,000 years have varied between approximately 350 and approximately 800 parts per 10(9) by volume (p.p.b.v.) during glacial and interglacial periods, respectively. In comparison, present-day methane levels of approximately 1,770 p.p.b.v. have been reported. Insights into the external forcing factors and internal feedbacks controlling atmospheric methane are essential for predicting the methane budget in a warmer world. Here we present a detailed atmospheric methane record from the EPICA Dome C ice core that extends the history of this greenhouse gas to 800,000 yr before present. The average time resolution of the new data is approximately 380 yr and permits the identification of orbital and millennial-scale features. Spectral analyses indicate that the long-term variability in atmospheric methane levels is dominated by approximately 100,000 yr glacial-interglacial cycles up to approximately 400,000 yr ago with an increasing contribution of the precessional component during the four more recent climatic cycles. We suggest that changes in the strength of tropical methane sources and sinks (wetlands, atmospheric oxidation), possibly influenced by changes in monsoon systems and the position of the intertropical convergence zone, controlled the atmospheric methane budget, with an additional source input during major terminations as the retreat of the northern ice sheet allowed higher methane emissions from extending periglacial wetlands. Millennial-scale changes in methane levels identified in our record as being associated with Antarctic isotope maxima events are indicative of ubiquitous millennial-scale temperature variability during the past eight glacial cycles.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Loulergue, Laetitia -- Schilt, Adrian -- Spahni, Renato -- Masson-Delmotte, Valerie -- Blunier, Thomas -- Lemieux, Benedicte -- Barnola, Jean-Marc -- Raynaud, Dominique -- Stocker, Thomas F -- Chappellaz, Jerome -- England -- Nature. 2008 May 15;453(7193):383-6. doi: 10.1038/nature06950.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Laboratoire de Glaciologie et Geophysique de l'Environnement, CNRS-Universite Joseph Fourier Grenoble, 54 Rue Moliere, 38402 St Martin d'Heres, France.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18480822" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/*chemistry ; Greenhouse Effect ; History, Ancient ; Ice Cover ; Methane/*analysis ; Temperature ; Time Factors ; Tropical Climate ; Wetlands
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  • 3
    Publication Date: 2008-10-31
    Description: Global amphibian declines have often been attributed to disease, but ignorance of the relative importance and mode of action of potential drivers of infection has made it difficult to develop effective remediation. In a field study, here we show that the widely used herbicide, atrazine, was the best predictor (out of more than 240 plausible candidates) of the abundance of larval trematodes (parasitic flatworms) in the declining northern leopard frog Rana pipiens. The effects of atrazine were consistent across trematode taxa. The combination of atrazine and phosphate--principal agrochemicals in global corn and sorghum production--accounted for 74% of the variation in the abundance of these often debilitating larval trematodes (atrazine alone accounted for 51%). Analysis of field data supported a causal mechanism whereby both agrochemicals increase exposure and susceptibility to larval trematodes by augmenting snail intermediate hosts and suppressing amphibian immunity. A mesocosm experiment demonstrated that, relative to control tanks, atrazine tanks had immunosuppressed tadpoles, had significantly more attached algae and snails, and had tadpoles with elevated trematode loads, further supporting a causal relationship between atrazine and elevated trematode infections in amphibians. These results raise concerns about the role of atrazine and phosphate in amphibian declines, and illustrate the value of quantifying the relative importance of several possible drivers of disease risk while determining the mechanisms by which they facilitate disease emergence.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Rohr, Jason R -- Schotthoefer, Anna M -- Raffel, Thomas R -- Carrick, Hunter J -- Halstead, Neal -- Hoverman, Jason T -- Johnson, Catherine M -- Johnson, Lucinda B -- Lieske, Camilla -- Piwoni, Marvin D -- Schoff, Patrick K -- Beasley, Val R -- England -- Nature. 2008 Oct 30;455(7217):1235-9. doi: 10.1038/nature07281.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Biology Department, University of South Florida, Tampa, Florida 33620, USA. jasonrohr@gmail.com〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18972018" target="_blank"〉PubMed〈/a〉
    Keywords: Agrochemicals/*pharmacology ; Animals ; Atrazine/pharmacology ; Biodiversity ; Disease Susceptibility/chemically induced/*veterinary ; Herbicides/pharmacology ; Larva/drug effects/physiology ; Phosphates/pharmacology ; Population Density ; Rana pipiens/immunology/*parasitology/*physiology ; Trematoda/*drug effects/growth & development/*physiology ; Trematode Infections/chemically induced/parasitology/*veterinary ; Wetlands
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  • 4
    Publication Date: 2008-07-25
    Description: Parasites can have strong impacts but are thought to contribute little biomass to ecosystems. We quantified the biomass of free-living and parasitic species in three estuaries on the Pacific coast of California and Baja California. Here we show that parasites have substantial biomass in these ecosystems. We found that parasite biomass exceeded that of top predators. The biomass of trematodes was particularly high, being comparable to that of the abundant birds, fishes, burrowing shrimps and polychaetes. Trophically transmitted parasites and parasitic castrators subsumed more biomass than did other parasitic functional groups. The extended phenotype biomass controlled by parasitic castrators sometimes exceeded that of their uninfected hosts. The annual production of free-swimming trematode transmission stages was greater than the combined biomass of all quantified parasites and was also greater than bird biomass. This biomass and productivity of parasites implies a profound role for infectious processes in these estuaries.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kuris, Armand M -- Hechinger, Ryan F -- Shaw, Jenny C -- Whitney, Kathleen L -- Aguirre-Macedo, Leopoldina -- Boch, Charlie A -- Dobson, Andrew P -- Dunham, Eleca J -- Fredensborg, Brian L -- Huspeni, Todd C -- Lorda, Julio -- Mababa, Luzviminda -- Mancini, Frank T -- Mora, Adrienne B -- Pickering, Maria -- Talhouk, Nadia L -- Torchin, Mark E -- Lafferty, Kevin D -- England -- Nature. 2008 Jul 24;454(7203):515-8. doi: 10.1038/nature06970.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Ecology, Evolution and Marine Biology and Marine Science Institute, University of California, Santa Barbara, California 93106, USA. kuris@lifesci.ucsb.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18650923" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; *Biomass ; California ; *Ecosystem ; Host-Parasite Interactions ; Pacific Ocean ; Parasites/*isolation & purification/*physiology ; Snails/parasitology ; Trematoda/isolation & purification/physiology ; Trematode Infections/parasitology ; Wetlands
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  • 5
    Publication Date: 2008-04-19
    Description: Past atmospheric methane concentrations show strong fluctuations in parallel to rapid glacial climate changes in the Northern Hemisphere superimposed on a glacial-interglacial doubling of methane concentrations. The processes driving the observed fluctuations remain uncertain but can be constrained using methane isotopic information from ice cores. Here we present an ice core record of carbon isotopic ratios in methane over the entire last glacial-interglacial transition. Our data show that the carbon in atmospheric methane was isotopically much heavier in cold climate periods. With the help of a box model constrained by the present data and previously published results, we are able to estimate the magnitude of past individual methane emission sources and the atmospheric lifetime of methane. We find that methane emissions due to biomass burning were about 45 Tg methane per year, and that these remained roughly constant throughout the glacial termination. The atmospheric lifetime of methane is reduced during cold climate periods. We also show that boreal wetlands are an important source of methane during warm events, but their methane emissions are essentially shut down during cold climate conditions.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Fischer, Hubertus -- Behrens, Melanie -- Bock, Michael -- Richter, Ulrike -- Schmitt, Jochen -- Loulergue, Laetitia -- Chappellaz, Jerome -- Spahni, Renato -- Blunier, Thomas -- Leuenberger, Markus -- Stocker, Thomas F -- England -- Nature. 2008 Apr 17;452(7189):864-7. doi: 10.1038/nature06825.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Alfred Wegener Institute for Polar and Marine Research, Columbusstrasse, 27568 Bremerhaven, Germany. hubertus.fischer@awi.de〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18421351" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/chemistry ; *Biomass ; Carbon/analysis ; Carbon Isotopes ; Cold Climate ; Fires/*statistics & numerical data ; Greenland ; History, Ancient ; Hydrogen/analysis ; *Ice Cover ; Methane/*analysis/*chemistry/metabolism ; Monte Carlo Method ; *Temperature ; Trees/*metabolism ; Wetlands
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  • 6
    Publication Date: 2009-12-17
    Description: Biota can be described in terms of elemental composition, expressed as an atomic ratio of carbon:nitrogen:phosphorus (refs 1-3). The elemental stoichiometry of microoorganisms is fundamental for understanding the production dynamics and biogeochemical cycles of ecosystems because microbial biomass is the trophic base of detrital food webs. Here we show that heterotrophic microbial communities of diverse composition from terrestrial soils and freshwater sediments share a common functional stoichiometry in relation to organic nutrient acquisition. The activities of four enzymes that catalyse the hydrolysis of assimilable products from the principal environmental sources of C, N and P show similar scaling relationships over several orders of magnitude, with a mean ratio for C:N:P activities near 1:1:1 in all habitats. We suggest that these ecoenzymatic ratios reflect the equilibria between the elemental composition of microbial biomass and detrital organic matter and the efficiencies of microbial nutrient assimilation and growth. Because ecoenzymatic activities intersect the stoichiometric and metabolic theories of ecology, they provide a functional measure of the threshold at which control of community metabolism shifts from nutrient to energy flow.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Sinsabaugh, Robert L -- Hill, Brian H -- Follstad Shah, Jennifer J -- England -- Nature. 2009 Dec 10;462(7274):795-8. doi: 10.1038/nature08632.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Biology Department, University of New Mexico, Albuquerque, New Mexico 871312, USA. rlsinsab@unm.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20010687" target="_blank"〉PubMed〈/a〉
    Keywords: Biomass ; Carbon/*metabolism ; *Ecosystem ; Enzyme Assays ; Enzymes/*metabolism ; Food Chain ; Geologic Sediments/*chemistry/microbiology ; Nitrogen/*metabolism ; Phosphorus/*metabolism ; Plants/metabolism ; Rivers ; *Soil Microbiology ; United States ; Wetlands
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  • 7
    Publication Date: 2012-08-24
    Description: After methane, ethane is the most abundant hydrocarbon in the remote atmosphere. It is a precursor to tropospheric ozone and it influences the atmosphere's oxidative capacity through its reaction with the hydroxyl radical, ethane's primary atmospheric sink. Here we present the longest continuous record of global atmospheric ethane levels. We show that global ethane emission rates decreased from 14.3 to 11.3 teragrams per year, or by 21 per cent, from 1984 to 2010. We attribute this to decreasing fugitive emissions from ethane's fossil fuel source--most probably decreased venting and flaring of natural gas in oil fields--rather than a decline in its other major sources, biofuel use and biomass burning. Ethane's major emission sources are shared with methane, and recent studies have disagreed on whether reduced fossil fuel or microbial emissions have caused methane's atmospheric growth rate to slow. Our findings suggest that reduced fugitive fossil fuel emissions account for at least 10-21 teragrams per year (30-70 per cent) of the decrease in methane's global emissions, significantly contributing to methane's slowing atmospheric growth rate since the mid-1980s.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Simpson, Isobel J -- Sulbaek Andersen, Mads P -- Meinardi, Simone -- Bruhwiler, Lori -- Blake, Nicola J -- Helmig, Detlev -- Rowland, F Sherwood -- Blake, Donald R -- England -- Nature. 2012 Aug 23;488(7412):490-4. doi: 10.1038/nature11342.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Chemistry, University of California-Irvine, Irvine, California 92697, USA. isimpson@uci.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22914166" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/*chemistry ; Biofuels/utilization ; Biomass ; Ethane/*analysis/*chemistry/history ; Greenhouse Effect ; History, 20th Century ; History, 21st Century ; Methane/*analysis/*chemistry/history ; Natural Gas/utilization ; Oil and Gas Fields ; Ozone/chemistry ; Wetlands
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  • 8
    Publication Date: 2013-12-07
    Description: The carbon cycle of the coastal ocean is a dynamic component of the global carbon budget. But the diverse sources and sinks of carbon and their complex interactions in these waters remain poorly understood. Here we discuss the sources, exchanges and fates of carbon in the coastal ocean and how anthropogenic activities have altered the carbon cycle. Recent evidence suggests that the coastal ocean may have become a net sink for atmospheric carbon dioxide during post-industrial times. Continued human pressures in coastal zones will probably have an important impact on the future evolution of the coastal ocean's carbon budget.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Bauer, James E -- Cai, Wei-Jun -- Raymond, Peter A -- Bianchi, Thomas S -- Hopkinson, Charles S -- Regnier, Pierre A G -- England -- Nature. 2013 Dec 5;504(7478):61-70. doi: 10.1038/nature12857.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Aquatic Biogeochemistry Laboratory, Department of Evolution, Ecology and Organismal Biology, The Ohio State University, Columbus, Ohio 43210, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24305149" target="_blank"〉PubMed〈/a〉
    Keywords: *Carbon Cycle ; Ecosystem ; Geologic Sediments ; Humans ; *Oceans and Seas ; Rivers/chemistry ; Wetlands
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  • 9
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    Nature Publishing Group (NPG)
    Publication Date: 2014-05-17
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Christensen, Torben R -- England -- Nature. 2014 May 15;509(7500):279-81.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24834515" target="_blank"〉PubMed〈/a〉
    Keywords: Arctic Regions ; Atmosphere/chemistry ; *Environmental Monitoring/economics/methods/standards ; Geologic Sediments/chemistry ; Global Warming/statistics & numerical data ; Greenhouse Effect/*statistics & numerical data ; Internationality ; Methane/adverse effects/*analysis ; Reference Standards ; Uncertainty ; Wetlands
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  • 10
    Publication Date: 2011-07-15
    Description: Increasing concentrations of atmospheric carbon dioxide (CO(2)) can affect biotic and abiotic conditions in soil, such as microbial activity and water content. In turn, these changes might be expected to alter the production and consumption of the important greenhouse gases nitrous oxide (N(2)O) and methane (CH(4)) (refs 2, 3). However, studies on fluxes of N(2)O and CH(4) from soil under increased atmospheric CO(2) have not been quantitatively synthesized. Here we show, using meta-analysis, that increased CO(2) (ranging from 463 to 780 parts per million by volume) stimulates both N(2)O emissions from upland soils and CH(4) emissions from rice paddies and natural wetlands. Because enhanced greenhouse-gas emissions add to the radiative forcing of terrestrial ecosystems, these emissions are expected to negate at least 16.6 per cent of the climate change mitigation potential previously predicted from an increase in the terrestrial carbon sink under increased atmospheric CO(2) concentrations. Our results therefore suggest that the capacity of land ecosystems to slow climate warming has been overestimated.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉van Groenigen, Kees Jan -- Osenberg, Craig W -- Hungate, Bruce A -- England -- Nature. 2011 Jul 13;475(7355):214-6. doi: 10.1038/nature10176.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Biological Sciences, Northern Arizona University, Flagstaff, Arizona 86011, USA. cjvangroenigen@nau.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21753852" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/*chemistry ; Carbon Dioxide/*analysis/metabolism ; Ecosystem ; Gases/*analysis ; Global Warming/statistics & numerical data ; *Greenhouse Effect/statistics & numerical data ; Methane/*analysis ; Nitrous Oxide/*analysis ; Oryza/growth & development ; Soil/analysis/*chemistry ; Wetlands
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  • 11
    Publication Date: 2011-08-13
    Description: Atmospheric methane (CH(4)) increased through much of the twentieth century, but this trend gradually weakened until a stable state was temporarily reached around the turn of the millennium, after which levels increased once more. The reasons for the slowdown are incompletely understood, with past work identifying changes in fossil fuel, wetland and agricultural sources and hydroxyl (OH) sinks as important causal factors. Here we show that the late-twentieth-century changes in the CH(4) growth rates are best explained by reduced microbial sources in the Northern Hemisphere. Our results, based on synchronous time series of atmospheric CH(4) mixing and (13)C/(12)C ratios and a two-box atmospheric model, indicate that the evolution of the mixing ratio requires no significant change in Southern Hemisphere sources between 1984 and 2005. Observed changes in the interhemispheric difference of (13)C effectively exclude reduced fossil fuel emissions as the primary cause of the slowdown. The (13)C observations are consistent with long-term reductions in agricultural emissions or another microbial source within the Northern Hemisphere. Approximately half (51 +/- 18%) of the decrease in Northern Hemisphere CH(4) emissions can be explained by reduced emissions from rice agriculture in Asia over the past three decades associated with increases in fertilizer application and reductions in water use.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kai, Fuu Ming -- Tyler, Stanley C -- Randerson, James T -- Blake, Donald R -- England -- Nature. 2011 Aug 10;476(7359):194-7. doi: 10.1038/nature10259.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth System Science, University of California, Irvine, California 92697, USA. fmkai@smart.mit.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21833086" target="_blank"〉PubMed〈/a〉
    Keywords: Agriculture/statistics & numerical data ; Animals ; Asia ; Atmosphere/*chemistry ; Biomass ; Fertilizers/utilization ; Fires ; Fossil Fuels/utilization ; *Geography ; Hydroxyl Radical/chemistry ; Methane/*analysis/metabolism ; Microbial Consortia/*physiology ; Oryza/metabolism ; Time Factors ; Water Supply/statistics & numerical data ; Wetlands
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  • 12
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    Nature Publishing Group (NPG)
    Publication Date: 2013-02-15
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Tollefson, Jeff -- England -- Nature. 2013 Feb 14;494(7436):162-4. doi: 10.1038/494162a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23407521" target="_blank"〉PubMed〈/a〉
    Keywords: *City Planning/economics/trends ; Climate Change/statistics & numerical data ; Cyclonic Storms/economics/mortality/statistics & numerical data ; *Disaster Planning/economics/trends ; Disasters/economics/*prevention & control/*statistics & numerical data ; Environmental Policy/economics/trends ; Floods/economics/*statistics & numerical data ; Humans ; New York City ; Risk Assessment ; Seawater/analysis ; Wetlands
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  • 13
    Publication Date: 2010-07-03
    Description: Terrestrial ecosystems gain carbon through photosynthesis and lose it mostly in the form of carbon dioxide (CO(2)). The extent to which the biosphere can act as a buffer against rising atmospheric CO(2) concentration in global climate change projections remains uncertain at the present stage. Biogeochemical theory predicts that soil nitrogen (N) scarcity may limit natural ecosystem response to elevated CO(2) concentration, diminishing the CO(2)-fertilization effect on terrestrial plant productivity in unmanaged ecosystems. Recent models have incorporated such carbon-nitrogen interactions and suggest that anthropogenic N sources could help sustain the future CO(2)-fertilization effect. However, conclusive demonstration that added N enhances plant productivity in response to CO(2)-fertilization in natural ecosystems remains elusive. Here we manipulated atmospheric CO(2) concentration and soil N availability in a herbaceous brackish wetland where plant community composition is dominated by a C(3) sedge and C(4) grasses, and is capable of responding rapidly to environmental change. We found that N addition enhanced the CO(2)-stimulation of plant productivity in the first year of a multi-year experiment, indicating N-limitation of the CO(2) response. But we also found that N addition strongly promotes the encroachment of C(4) plant species that respond less strongly to elevated CO(2) concentrations. Overall, we found that the observed shift in the plant community composition ultimately suppresses the CO(2)-stimulation of plant productivity by the third and fourth years. Although extensive research has shown that global change factors such as elevated CO(2) concentrations and N pollution affect plant species differently and that they may drive plant community changes, we demonstrate that plant community shifts can act as a feedback effect that alters the whole ecosystem response to elevated CO(2) concentrations. Moreover, we suggest that trade-offs between the abilities of plant taxa to respond positively to different perturbations may constrain natural ecosystem response to global change.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Langley, J Adam -- Megonigal, J Patrick -- England -- Nature. 2010 Jul 1;466(7302):96-9. doi: 10.1038/nature09176.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Smithsonian Environmental Research Center, Edgewater, Maryland 21037, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20596018" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/analysis/chemistry ; Biomass ; Carbon Dioxide/analysis/*metabolism ; *Ecosystem ; Human Activities ; Nitrogen/*metabolism ; Plant Development ; Plants/*metabolism ; Poaceae/growth & development/metabolism ; Rivers ; Soil/analysis ; Water/analysis ; Wetlands
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  • 14
    Publication Date: 2011-03-04
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Qiu, Jane -- England -- Nature. 2011 Mar 3;471(7336):19. doi: 10.1038/471019a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21368798" target="_blank"〉PubMed〈/a〉
    Keywords: China ; Conservation of Natural Resources/economics/*trends ; Ecology/methods/trends ; *Ecosystem ; Environmental Policy/economics/*trends ; Water Supply ; Wetlands
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 15
    Publication Date: 2012-03-03
    Description: The origin of trees by the mid-Devonian epoch (398-385 million years ago) signals a major change in terrestrial ecosystems with potential long-term consequences including increased weathering, drop in atmospheric CO(2), modified climate, changes in sedimentation patterns and mass extinction. However, little is known about the ecology of early forests or how changes in early terrestrial ecosystems influenced global processes. One of the most famous palaeontological records for this time is the 'oldest fossil forest' at Riverside Quarry, Gilboa, New York, USA, discovered in the 1920s. Hundreds of large Eospermatopteris sandstone casts, now thought to represent the bases of standing cladoxylopsid trees, were recovered from a horizon that was originally interpreted as a muddy swamp. After quarry operations ceased, relatively minor outcrops of similar fossils at nearby localities have provided limited opportunities to evaluate this pervasive view using modern methods. In 2010, removal of the quarry backfill enabled reappraisal of the palaeoecology of this important site. Here we describe a 1,200 m(2) map showing numerous Eospermatopteris root systems in life position within a mixed-age stand of trees. Unexpectedly, large woody rhizomes with adventitious roots and aerial branch systems identified as aneurophytalean progymnosperms run between, and probably climb into, Eospermatopteris trees. We describe the overall habit for these surprisingly large aneurophytaleans, the earliest fossil group having wood produced by a bifacial vascular cambium. The site also provides evidence for arborescence within lycopsids, extending the North American range for trees in this ecologically critical group. The rooting horizon is a dark grey sandy mudstone showing limited root penetration. Although clearly belonging to a wetland coastal plain environment, the forest was probably limited in duration and subject to periodic disturbance. These observations provide fundamental clarification of the palaeoecology of this mixed-group early forest, with important implications for interpreting coeval assemblage data worldwide.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Stein, William E -- Berry, Christopher M -- Hernick, Linda VanAller -- Mannolini, Frank -- England -- Nature. 2012 Feb 29;483(7387):78-81. doi: 10.1038/nature10819.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Biological Sciences, Binghamton University, New York, NY 13902-6000, USA. stein@binghamton.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22382983" target="_blank"〉PubMed〈/a〉
    Keywords: *Biodiversity ; Cambium/metabolism ; Extraction and Processing Industry ; *Fossils ; New York ; Plant Roots/anatomy & histology/physiology ; Rhizome/anatomy & histology/physiology ; Soil/analysis/chemistry ; Trees/anatomy & histology/*physiology ; Wetlands ; Wood/metabolism
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    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 16
    Publication Date: 2014-03-29
    Description: Methane (CH4) is an important greenhouse gas because it has 25 times the global warming potential of carbon dioxide (CO2) by mass over a century. Recent calculations suggest that atmospheric CH4 emissions have been responsible for approximately 20% of Earth's warming since pre-industrial times. Understanding how CH4 emissions from ecosystems will respond to expected increases in global temperature is therefore fundamental to predicting whether the carbon cycle will mitigate or accelerate climate change. Methanogenesis is the terminal step in the remineralization of organic matter and is carried out by strictly anaerobic Archaea. Like most other forms of metabolism, methanogenesis is temperature-dependent. However, it is not yet known how this physiological response combines with other biotic processes (for example, methanotrophy, substrate supply, microbial community composition) and abiotic processes (for example, water-table depth) to determine the temperature dependence of ecosystem-level CH4 emissions. It is also not known whether CH4 emissions at the ecosystem level have a fundamentally different temperature dependence than other key fluxes in the carbon cycle, such as photosynthesis and respiration. Here we use meta-analyses to show that seasonal variations in CH4 emissions from a wide range of ecosystems exhibit an average temperature dependence similar to that of CH4 production derived from pure cultures of methanogens and anaerobic microbial communities. This average temperature dependence (0.96 electron volts (eV)), which corresponds to a 57-fold increase between 0 and 30 degrees C, is considerably higher than previously observed for respiration (approximately 0.65 eV) and photosynthesis (approximately 0.3 eV). As a result, we show that both the emission of CH4 and the ratio of CH4 to CO2 emissions increase markedly with seasonal increases in temperature. Our findings suggest that global warming may have a large impact on the relative contributions of CO2 and CH4 to total greenhouse gas emissions from aquatic ecosystems, terrestrial wetlands and rice paddies.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Yvon-Durocher, Gabriel -- Allen, Andrew P -- Bastviken, David -- Conrad, Ralf -- Gudasz, Cristian -- St-Pierre, Annick -- Thanh-Duc, Nguyen -- del Giorgio, Paul A -- England -- Nature. 2014 Mar 27;507(7493):488-91. doi: 10.1038/nature13164. Epub 2014 Mar 19.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Environment and Sustainability Institute, University of Exeter, Penryn, Cornwall, TR10 9EZ. UK. ; Department of Biological Sciences, Macquarie University, Sydney, NSW 2109, Australia. ; Department of Thematic Studies - Water and Environmental Studies, Linkoping University, SE-581 83 Linkoping, Sweden. ; Max-Planck-Institute for Terrestrial Microbiology, Karl-von-Frisch-Strasse 10, 35043 Marburg, Germany. ; 1] Department of Ecology and Environmental Sciences, Umea University, Linnaeus vag 6, SE-901 87 Umea, Sweden [2] Department of Ecology and Genetics, Limnology, Uppsala University, Norbyvagen 18D, SE-752 36, Uppsala Sweden [3] Department of Ecology and Evolutionary Biology, Princeton University, Princeton, 106A Guyot Hall, New Jersey 08544, USA. ; Departement des sciences biologiques, Universite du Quebec a Montreal, Montreal, Province of Quebec, H2X 3X8, Canada. ; Earth Systems Research Center, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, New Hampshire 03824, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24670769" target="_blank"〉PubMed〈/a〉
    Keywords: Anaerobiosis ; Aquatic Organisms/metabolism ; Archaea/*metabolism ; Atmosphere/chemistry ; Carbon Cycle ; Carbon Dioxide/analysis ; Cell Respiration ; *Ecosystem ; Geologic Sediments/microbiology ; *Global Warming ; Greenhouse Effect ; Methane/analysis/*metabolism ; Oryza/metabolism ; Photosynthesis ; Seasons ; *Temperature ; Wetlands
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    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 17
    Publication Date: 2014-10-25
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Jun, Chen -- Ban, Yifang -- Li, Songnian -- England -- Nature. 2014 Oct 23;514(7523):434. doi: 10.1038/514434c.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉National Geomatics Center of China, Beijing, China. ; KTH Royal Institute of Technology, Stockholm, Sweden. ; Ryerson University, Toronto, Ontario, Canada.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25341776" target="_blank"〉PubMed〈/a〉
    Keywords: *Access to Information ; China ; Conservation of Natural Resources/methods ; *Earth (Planet) ; Forests ; Information Dissemination ; *Maps as Topic ; *Satellite Imagery ; United Nations ; Wetlands
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    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 18
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    Nature Publishing Group (NPG)
    Publication Date: 2015-09-04
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉England -- Nature. 2015 Sep 3;525(7567):5. doi: 10.1038/525005b.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26333434" target="_blank"〉PubMed〈/a〉
    Keywords: Agricultural Irrigation/methods/trends ; Animals ; Birds ; California ; Droughts/*statistics & numerical data ; Ecology/methods/*trends ; *Ecosystem ; Fires ; Fishes ; Groundwater/analysis ; *Water Supply/analysis/statistics & numerical data ; Wetlands
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 19
    Publication Date: 2016-03-25
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kindlmann, Pavel -- Krenova, Zdenka -- England -- Nature. 2016 Mar 24;531(7595):448. doi: 10.1038/531448d.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Global Change Research Institute, Brno; and Charles University, Prague, Czech Republic.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/27008958" target="_blank"〉PubMed〈/a〉
    Keywords: *Biodiversity ; Conservation of Natural Resources/*legislation & jurisprudence ; Czech Republic ; Endangered Species/legislation & jurisprudence ; Forests ; Parks, Recreational/*legislation & jurisprudence ; Wetlands
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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