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  • 2010-2014  (20)
  • Chemistry and Pharmacology  (20)
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  • 1
    Publication Date: 2010-08-28
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Machlis, Gary E -- McNutt, Marcia K -- New York, N.Y. -- Science. 2010 Aug 27;329(5995):1018-9. doi: 10.1126/science.1195382.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Strategic Sciences Working Group, U.S. Department of the Interior, Washington, DC 20024, USA. gary_machlis@nps.gov〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20798302" target="_blank"〉PubMed〈/a〉
    Keywords: *Accidents ; Animals ; Atlantic Ocean ; Decision Making ; *Disasters ; *Ecosystem ; Environmental Pollution ; Fisheries ; Forecasting ; Interdisciplinary Communication ; *Petroleum ; Planning Techniques ; Public Policy ; United States ; United States Government Agencies ; Wetlands
    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: 2010-05-22
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kerr, Richard A -- Kintisch, Eli -- Schenkman, Lauren -- Stokstad, Erik -- New York, N.Y. -- Science. 2010 May 21;328(5981):962-3. doi: 10.1126/science.328.5981.962.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20489000" target="_blank"〉PubMed〈/a〉
    Keywords: *Accidents ; Animals ; Atlantic Ocean ; *Disasters ; *Ecosystem ; Environmental Monitoring ; *Environmental Pollution ; Fisheries ; Food Chain ; *Petroleum ; Plants ; Wetlands
    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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  • 3
    Publication Date: 2010-11-13
    Description: The Amazonian rainforest is arguably the most species-rich terrestrial ecosystem in the world, yet the timing of the origin and evolutionary causes of this diversity are a matter of debate. We review the geologic and phylogenetic evidence from Amazonia and compare it with uplift records from the Andes. This uplift and its effect on regional climate fundamentally changed the Amazonian landscape by reconfiguring drainage patterns and creating a vast influx of sediments into the basin. On this "Andean" substrate, a region-wide edaphic mosaic developed that became extremely rich in species, particularly in Western Amazonia. We show that Andean uplift was crucial for the evolution of Amazonian landscapes and ecosystems, and that current biodiversity patterns are rooted deep in the pre-Quaternary.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Hoorn, C -- Wesselingh, F P -- ter Steege, H -- Bermudez, M A -- Mora, A -- Sevink, J -- Sanmartin, I -- Sanchez-Meseguer, A -- Anderson, C L -- Figueiredo, J P -- Jaramillo, C -- Riff, D -- Negri, F R -- Hooghiemstra, H -- Lundberg, J -- Stadler, T -- Sarkinen, T -- Antonelli, A -- New York, N.Y. -- Science. 2010 Nov 12;330(6006):927-31. doi: 10.1126/science.1194585.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Paleoecology and Landscape Ecology, Institute for Biodiversity and Ecosystem Dynamics (IBED), University of Amsterdam, Science Park 904, 1098 XH Amsterdam, Netherlands. carina.hoorn@milne.cc〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21071659" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; *Biodiversity ; *Climate Change ; Ecosystem ; Fossils ; Geography ; *Geological Phenomena ; Phylogeny ; Rivers ; South America ; Time ; Trees ; Wetlands
    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
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2010-12-18
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Stokstad, Erik -- New York, N.Y. -- Science. 2010 Dec 17;330(6011):1608. doi: 10.1126/science.330.6011.1608-a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21163982" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Ecosystem ; *Environmental Pollution ; *Petroleum ; Wetlands
    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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  • 5
    Publication Date: 2013-04-06
    Description: Ice cores from low latitudes can provide a wealth of unique information about past climate in the tropics, but they are difficult to recover and few exist. Here, we report annually resolved ice core records from the Quelccaya ice cap (5670 meters above sea level) in Peru that extend back ~1800 years and provide a high-resolution record of climate variability there. Oxygen isotopic ratios (delta(18)O) are linked to sea surface temperatures in the tropical eastern Pacific, whereas concentrations of ammonium and nitrate document the dominant role played by the migration of the Intertropical Convergence Zone in the region of the tropical Andes. Quelccaya continues to retreat and thin. Radiocarbon dates on wetland plants exposed along its retreating margins indicate that it has not been smaller for at least six millennia.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Thompson, L G -- Mosley-Thompson, E -- Davis, M E -- Zagorodnov, V S -- Howat, I M -- Mikhalenko, V N -- Lin, P-N -- New York, N.Y. -- Science. 2013 May 24;340(6135):945-50. doi: 10.1126/science.1234210. Epub 2013 Apr 4.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Byrd Polar Research Center, The Ohio State University, Columbus, OH 43210, USA. thompson.3@osu.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23558172" target="_blank"〉PubMed〈/a〉
    Keywords: *Climate Change ; *Ice Cover ; Nitrates/analysis ; Oxygen Isotopes/analysis ; Peru ; Plants ; Quaternary Ammonium Compounds/analysis ; *Tropical Climate ; Wetlands
    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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  • 6
    Publication Date: 2014-08-26
    Description: Carbon in thawing permafrost soils may have global impacts on climate change; however, the factors that control its processing and fate are poorly understood. The dominant fate of dissolved organic carbon (DOC) released from soils to inland waters is either complete oxidation to CO2 or partial oxidation and river export to oceans. Although both processes are most often attributed to bacterial respiration, we found that photochemical oxidation exceeds rates of respiration and accounts for 70 to 95% of total DOC processed in the water column of arctic lakes and rivers. At the basin scale, photochemical processing of DOC is about one-third of the total CO2 released from surface waters and is thus an important component of the arctic carbon budget.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Cory, Rose M -- Ward, Collin P -- Crump, Byron C -- Kling, George W -- New York, N.Y. -- Science. 2014 Aug 22;345(6199):925-8. doi: 10.1126/science.1253119.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI 48109, USA. rmcory@umich.edu. ; Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI 48109, USA. ; Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA. ; Department of Ecology and Evolutionary Biology, University of Michigan, Ann Arbor, MI 48109, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25146289" target="_blank"〉PubMed〈/a〉
    Keywords: Arctic Regions ; Carbon/*chemistry ; *Carbon Cycle ; Carbon Dioxide/chemistry ; Fresh Water/*chemistry ; Geologic Sediments/chemistry ; Photochemical Processes ; Soil ; *Sunlight ; Wetlands
    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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  • 7
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2014-02-01
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Nisbet, Euan G -- Dlugokencky, Edward J -- Bousquet, Philippe -- New York, N.Y. -- Science. 2014 Jan 31;343(6170):493-5. doi: 10.1126/science.1247828.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth Sciences, Royal Holloway, University of London, Egham TW20 0EX, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24482471" target="_blank"〉PubMed〈/a〉
    Keywords: Air ; Atmosphere/*chemistry ; *Climate Change ; Coal ; Geography ; Greenhouse Effect/prevention & control ; Humans ; Industry ; Methane/*analysis ; Seasons ; Wetlands
    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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  • 8
    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
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 9
    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
    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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    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
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 11
    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
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 12
    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
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 13
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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
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 14
    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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    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 15
    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
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    Electronic ISSN: 1476-4687
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  • 16
    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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    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 17
    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
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 18
    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
    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: 2010-05-08
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kerr, Richard -- Kintisch, Eli -- Stokstad, Erik -- New York, N.Y. -- Science. 2010 May 7;328(5979):674-5. doi: 10.1126/science.328.5979.674.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20448155" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; *Disasters ; *Ecosystem ; Environmental Pollution ; *Environmental Restoration and Remediation ; Fisheries ; *Petroleum ; United States ; *Water Pollution ; Wetlands
    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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  • 20
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2013-02-23
    Description: Shallow groundwater affects terrestrial ecosystems by sustaining river base-flow and root-zone soil water in the absence of rain, but little is known about the global patterns of water table depth and where it provides vital support for land ecosystems. We present global observations of water table depth compiled from government archives and literature, and fill in data gaps and infer patterns and processes using a groundwater model forced by modern climate, terrain, and sea level. Patterns in water table depth explain patterns in wetlands at the global scale and vegetation gradients at regional and local scales. Overall, shallow groundwater influences 22 to 32% of global land area, including ~15% as groundwater-fed surface water features and 7 to 17% with the water table or its capillary fringe within plant rooting depths.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Fan, Y -- Li, H -- Miguez-Macho, G -- New York, N.Y. -- Science. 2013 Feb 22;339(6122):940-3. doi: 10.1126/science.1229881.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth and Planetary Sciences, Rutgers University, New Brunswick, NJ 08854, USA. yingfan@rci.rutgers.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23430651" target="_blank"〉PubMed〈/a〉
    Keywords: Climate ; *Ecosystem ; Geography ; *Groundwater ; Models, Theoretical ; Plants ; Rain ; Rivers ; Wetlands
    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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