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  • Photosynthesis
  • Nature Publishing Group (NPG)  (31)
  • American Institute of Physics (AIP)
  • Elsevier
  • 2010-2014  (31)
  • 1
    Publication Date: 2010-11-12
    Description: Geochemical data from ancient sedimentary successions provide evidence for the progressive evolution of Earth's atmosphere and oceans. Key stages in increasing oxygenation are postulated for the Palaeoproterozoic era ( approximately 2.3 billion years ago, Gyr ago) and the late Proterozoic eon (about 0.8 Gyr ago), with the latter implicated in the subsequent metazoan evolutionary expansion. In support of this rise in oxygen concentrations, a large database shows a marked change in the bacterially mediated fractionation of seawater sulphate to sulphide of Delta(34)S 〈 25 per thousand before 1 Gyr to 〉/=50 per thousand after 0.64 Gyr. This change in Delta(34)S has been interpreted to represent the evolution from single-step bacterial sulphate reduction to a combination of bacterial sulphate reduction and sulphide oxidation, largely bacterially mediated. This evolution is seen as marking the rise in atmospheric oxygen concentrations and the evolution of non-photosynthetic sulphide-oxidizing bacteria. Here we report Delta(34)S values exceeding 50 per thousand from a terrestrial Mesoproterozoic (1.18 Gyr old) succession in Scotland, a time period that is at present poorly characterized. This level of fractionation implies disproportionation in the sulphur cycle, probably involving sulphide-oxidizing bacteria, that is not evident from Delta(34)S data in the marine record. Disproportionation in both red beds and lacustrine black shales at our study site suggests that the Mesoproterozoic terrestrial environment was sufficiently oxygenated to support a biota that was adapted to an oxygen-rich atmosphere, but had also penetrated into subsurface sediment.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Parnell, John -- Boyce, Adrian J -- Mark, Darren -- Bowden, Stephen -- Spinks, Sam -- England -- Nature. 2010 Nov 11;468(7321):290-3. doi: 10.1038/nature09538.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉School of Geosciences, University of Aberdeen, Aberdeen AB24 3UE, UK. j.parnell@abdn.ac.uk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21068840" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/chemistry ; Bacteria/metabolism ; Geologic Sediments/*chemistry/microbiology ; History, Ancient ; Iron/analysis/chemistry ; Oxidation-Reduction ; Oxygen/analysis/*metabolism ; Photosynthesis ; Scotland ; Seawater/chemistry ; Sulfates/metabolism ; Sulfides/analysis/chemistry/metabolism
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  • 2
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    Nature Publishing Group (NPG)
    Publication Date: 2010-12-15
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Vedral, Vlatko -- England -- Nature. 2010 Dec 9;468(7325):769-70. doi: 10.1038/468769a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21150986" target="_blank"〉PubMed〈/a〉
    Keywords: Hot Temperature ; Models, Biological ; Photosynthesis ; *Quantum Theory ; *Thermodynamics
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  • 3
    Publication Date: 2014-12-10
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Gruber, Nicolas -- England -- Nature. 2015 Jan 8;517(7533):148-9. doi: 10.1038/nature14082. Epub 2014 Dec 10.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Environmental Physics Group, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zurich, 8092 Zurich, Switzerland.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25487156" target="_blank"〉PubMed〈/a〉
    Keywords: Aquatic Organisms/metabolism ; Atmosphere/chemistry ; Carbon Dioxide/*analysis ; *Carbon Sequestration ; *Ecosystem ; Human Activities ; *Oceans and Seas ; Photosynthesis
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  • 4
    Publication Date: 2012-03-02
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Falkowski, Paul -- England -- Nature. 2012 Feb 29;483(7387):S21. doi: 10.1038/483S21a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22378124" target="_blank"〉PubMed〈/a〉
    Keywords: Aquatic Organisms/*metabolism ; Environmental Restoration and Remediation ; Eutrophication ; Extinction, Biological ; *Global Warming ; *Human Activities ; Interdisciplinary Studies ; Marine Biology ; Photosynthesis ; Phytoplankton/*metabolism ; Seawater/chemistry/microbiology ; Time Factors
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  • 5
    Publication Date: 2012-04-27
    Description: The phenology of growth in temperate deciduous forests, including the timing of leaf emergence and senescence, has strong control over ecosystem properties such as productivity and nutrient cycling, and has an important role in the carbon economy of understory plants. Extended leaf phenology, whereby understory species assimilate carbon in early spring before canopy closure or in late autumn after canopy fall, has been identified as a key feature of many forest species invasions, but it remains unclear whether there are systematic differences in the growth phenology of native and invasive forest species or whether invaders are more responsive to warming trends that have lengthened the duration of spring or autumn growth. Here, in a 3-year monitoring study of 43 native and 30 non-native shrub and liana species common to deciduous forests in the eastern United States, I show that extended autumn leaf phenology is a common attribute of eastern US forest invasions, where non-native species are extending the autumn growing season by an average of 4 weeks compared with natives. In contrast, there was no consistent evidence that non-natives as a group show earlier spring growth phenology, and non-natives were not better able to track interannual variation in spring temperatures. Seasonal leaf production and photosynthetic data suggest that most non-native species capture a significant proportion of their annual carbon assimilate after canopy leaf fall, a behaviour that was virtually absent in natives and consistent across five phylogenetic groups. Pronounced differences in how native and non-native understory species use pre- and post-canopy environments suggest eastern US invaders are driving a seasonal redistribution of forest productivity that may rival climate change in its impact on forest processes.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Fridley, Jason D -- England -- Nature. 2012 May 17;485(7398):359-62. doi: 10.1038/nature11056.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Biology, Syracuse University, 107 College Place, Syracuse, New York 13244, USA. fridley@syr.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22535249" target="_blank"〉PubMed〈/a〉
    Keywords: Carbon/metabolism ; *Ecosystem ; *Introduced Species ; Photosynthesis ; Plant Leaves/classification/*growth & development ; *Seasons ; Temperature ; Time Factors ; Trees/classification/*growth & development ; United States
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  • 6
    Publication Date: 2012-03-20
    Description: Two decades of scientific ocean drilling have demonstrated widespread microbial life in deep sub-seafloor sediment, and surprisingly high microbial-cell numbers. Despite the ubiquity of life in the deep biosphere, the large community sizes and the low energy fluxes in this vast buried ecosystem are not yet understood. It is not known whether organisms of the deep biosphere are specifically adapted to extremely low energy fluxes or whether most of the observed cells are in a dormant, spore-like state. Here we apply a new approach--the D:L-amino-acid model--to quantify the distributions and turnover times of living microbial biomass, endospores and microbial necromass, as well as to determine their role in the sub-seafloor carbon budget. The approach combines sensitive analyses of unique bacterial markers (muramic acid and D-amino acids) and the bacterial endospore marker, dipicolinic acid, with racemization dynamics of stereo-isomeric amino acids. Endospores are as abundant as vegetative cells and microbial activity is extremely low, leading to microbial biomass turnover times of hundreds to thousands of years. We infer from model calculations that biomass production is sustained by organic carbon deposited from the surface photosynthetic world millions of years ago and that microbial necromass is recycled over timescales of hundreds of thousands of years.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Lomstein, Bente Aa -- Langerhuus, Alice T -- D'Hondt, Steven -- Jorgensen, Bo B -- Spivack, Arthur J -- England -- Nature. 2012 Mar 18;484(7392):101-4. doi: 10.1038/nature10905.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Bioscience, Section for Microbiology, Aarhus University, Building 1540, Ny Munkegade 114, DK-8000 Aarhus C, Denmark. bente.lomstein@biology.au.dk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22425999" target="_blank"〉PubMed〈/a〉
    Keywords: Altitude ; Amino Acids/analysis/chemistry/metabolism ; Aquatic Organisms/chemistry/growth & development/*isolation & purification ; Archaea/chemistry/cytology/*growth & development/isolation & purification ; Bacteria/chemistry/cytology/*growth & development/isolation & purification ; Biomarkers/analysis ; *Biomass ; Carbon/metabolism ; Cell Wall/chemistry ; Geologic Sediments/*microbiology ; Muramic Acids/analysis ; Oceans and Seas ; Oxidation-Reduction ; Peru ; Photosynthesis ; Picolinic Acids/analysis ; Seawater/*microbiology ; Spores, Bacterial/chemistry/growth & development/isolation & purification ; Time Factors
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  • 7
    Publication Date: 2013-05-17
    Description: High latitudes contain nearly half of global soil carbon, prompting interest in understanding how the Arctic terrestrial carbon balance will respond to rising temperatures. Low temperatures suppress the activity of soil biota, retarding decomposition and nitrogen release, which limits plant and microbial growth. Warming initially accelerates decomposition, increasing nitrogen availability, productivity and woody-plant dominance. However, these responses may be transitory, because coupled abiotic-biotic feedback loops that alter soil-temperature dynamics and change the structure and activity of soil communities, can develop. Here we report the results of a two-decade summer warming experiment in an Alaskan tundra ecosystem. Warming increased plant biomass and woody dominance, indirectly increased winter soil temperature, homogenized the soil trophic structure across horizons and suppressed surface-soil-decomposer activity, but did not change total soil carbon or nitrogen stocks, thereby increasing net ecosystem carbon storage. Notably, the strongest effects were in the mineral horizon, where warming increased decomposer activity and carbon stock: a 'biotic awakening' at depth.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Sistla, Seeta A -- Moore, John C -- Simpson, Rodney T -- Gough, Laura -- Shaver, Gaius R -- Schimel, Joshua P -- England -- Nature. 2013 May 30;497(7451):615-8. doi: 10.1038/nature12129. Epub 2013 May 15.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Ecology, Evolution and Marine Biology, University of California Santa Barbara, Santa Barbara, California 93108, USA. sistla@lifesci.ucsb.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23676669" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Arctic Regions ; Biomass ; Carbon/*analysis ; *Carbon Cycle ; *Cold Climate ; Discriminant Analysis ; *Ecosystem ; Food Chain ; Global Warming/*statistics & numerical data ; History, 20th Century ; History, 21st Century ; Nitrogen/metabolism ; Photosynthesis ; Plants/metabolism ; Rain ; Soil/analysis/*chemistry/parasitology ; Soil Microbiology ; *Temperature ; Time Factors ; Uncertainty
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  • 8
    Publication Date: 2013-04-05
    Description: The technological demand to push the gigahertz (10(9) hertz) switching speed limit of today's magnetic memory and logic devices into the terahertz (10(12) hertz) regime underlies the entire field of spin-electronics and integrated multi-functional devices. This challenge is met by all-optical magnetic switching based on coherent spin manipulation. By analogy to femtosecond chemistry and photosynthetic dynamics--in which photoproducts of chemical and biochemical reactions can be influenced by creating suitable superpositions of molecular states--femtosecond-laser-excited coherence between electronic states can switch magnetic order by 'suddenly' breaking the delicate balance between competing phases of correlated materials: for example, manganites exhibiting colossal magneto-resistance suitable for applications. Here we show femtosecond (10(-15) seconds) photo-induced switching from antiferromagnetic to ferromagnetic ordering in Pr0.7Ca0.3MnO3, by observing the establishment (within about 120 femtoseconds) of a huge temperature-dependent magnetization with photo-excitation threshold behaviour absent in the optical reflectivity. The development of ferromagnetic correlations during the femtosecond laser pulse reveals an initial quantum coherent regime of magnetism, distinguished from the picosecond (10(-12) seconds) lattice-heating regime characterized by phase separation without threshold behaviour. Our simulations reproduce the nonlinear femtosecond spin generation and underpin fast quantum spin-flip fluctuations correlated with coherent superpositions of electronic states to initiate local ferromagnetic correlations. These results merge two fields, femtosecond magnetism in metals and band insulators, and non-equilibrium phase transitions of strongly correlated electrons, in which local interactions exceeding the kinetic energy produce a complex balance of competing orders.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Li, Tianqi -- Patz, Aaron -- Mouchliadis, Leonidas -- Yan, Jiaqiang -- Lograsso, Thomas A -- Perakis, Ilias E -- Wang, Jigang -- England -- Nature. 2013 Apr 4;496(7443):69-73. doi: 10.1038/nature11934.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Physics and Astronomy, Iowa State University, Ames, Iowa 50011, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23552945" target="_blank"〉PubMed〈/a〉
    Keywords: Biology ; Chemistry ; Circular Dichroism ; Electronics ; Iron/chemistry ; *Magnetic Phenomena ; Magnetics ; Optics and Photonics ; Photosynthesis ; *Quantum Theory ; Temperature ; Time Factors
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  • 9
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    Nature Publishing Group (NPG)
    Publication Date: 2013-10-18
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉England -- Nature. 2013 Oct 17;502(7471):S60-1. doi: 10.1038/502S60a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24132337" target="_blank"〉PubMed〈/a〉
    Keywords: Biofuels/adverse effects/economics ; Biomass ; Climate Change/statistics & numerical data ; Photosynthesis ; *Renewable Energy/economics ; Solar Energy/economics ; Technology/economics/*trends
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  • 10
    Publication Date: 2013-02-08
    Description: The release of carbon from tropical forests may exacerbate future climate change, but the magnitude of the effect in climate models remains uncertain. Coupled climate-carbon-cycle models generally agree that carbon storage on land will increase as a result of the simultaneous enhancement of plant photosynthesis and water use efficiency under higher atmospheric CO(2) concentrations, but will decrease owing to higher soil and plant respiration rates associated with warming temperatures. At present, the balance between these effects varies markedly among coupled climate-carbon-cycle models, leading to a range of 330 gigatonnes in the projected change in the amount of carbon stored on tropical land by 2100. Explanations for this large uncertainty include differences in the predicted change in rainfall in Amazonia and variations in the responses of alternative vegetation models to warming. Here we identify an emergent linear relationship, across an ensemble of models, between the sensitivity of tropical land carbon storage to warming and the sensitivity of the annual growth rate of atmospheric CO(2) to tropical temperature anomalies. Combined with contemporary observations of atmospheric CO(2) concentration and tropical temperature, this relationship provides a tight constraint on the sensitivity of tropical land carbon to climate change. We estimate that over tropical land from latitude 30 degrees north to 30 degrees south, warming alone will release 53 +/- 17 gigatonnes of carbon per kelvin. Compared with the unconstrained ensemble of climate-carbon-cycle projections, this indicates a much lower risk of Amazon forest dieback under CO(2)-induced climate change if CO(2) fertilization effects are as large as suggested by current models. Our study, however, also implies greater certainty that carbon will be lost from tropical land if warming arises from reductions in aerosols or increases in other greenhouse gases.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Cox, Peter M -- Pearson, David -- Booth, Ben B -- Friedlingstein, Pierre -- Huntingford, Chris -- Jones, Chris D -- Luke, Catherine M -- England -- Nature. 2013 Feb 21;494(7437):341-4. doi: 10.1038/nature11882. Epub 2013 Feb 6.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉College of Engineering, Mathematics and Physical Science, University of Exeter, Exeter EX4 4QF, UK. p.m.cox@exeter.ac.uk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23389447" target="_blank"〉PubMed〈/a〉
    Keywords: Carbon Cycle/*physiology ; Carbon Dioxide/analysis/*metabolism ; Cell Respiration ; *Climate Change ; *Models, Theoretical ; Photosynthesis ; Rain ; Temperature ; Trees/*metabolism ; *Tropical Climate ; Uncertainty
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  • 11
    Publication Date: 2013-08-30
    Description: Coccolithophores are marine algae that use carbon for calcification and photosynthesis. The long-term adaptation of these and other marine algae to decreasing carbon dioxide levels during the Cenozoic era has resulted in modern algae capable of actively enhancing carbon dioxide at the site of photosynthesis. This enhancement occurs through the transport of dissolved bicarbonate (HCO3(-)) and with the help of enzymes whose expression can be modulated by variable aqueous carbon dioxide concentration, [CO2], in laboratory cultures. Coccolithophores preserve the geological history of this adaptation because the stable carbon and oxygen isotopic compositions of their calcite plates (coccoliths), which are preserved in the fossil record, are sensitive to active carbon uptake and transport by the cell. Here we use a model of cellular carbon fluxes and show that at low [CO2] the increased demand for HCO3(-) at the site of photosynthesis results in a diminished allocation of HCO3(-) to calcification, which is most pronounced in larger cells. This results in a large divergence between the carbon isotopic compositions of small versus large coccoliths only at low [CO2]. Our evaluation of the oxygen and carbon isotope record of size-separated fossil coccoliths reveals that this isotopic divergence first arose during the late Miocene to the earliest Pliocene epoch (about 7-5 million years ago). We interpret this to be a threshold response of the cells' carbon acquisition strategies to decreasing [CO2]. The documented coccolithophore response is synchronous with a global shift in terrestrial vegetation distribution between 8 and 5 Myr ago, which has been interpreted by some studies as a floral response to decreasing partial pressures of carbon dioxide () in the atmosphere. We infer a global decrease in carbon dioxide levels for this time interval that has not yet been identified in the sparse proxy record but is synchronous with global cooling and progressive glaciations.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Bolton, Clara T -- Stoll, Heather M -- England -- Nature. 2013 Aug 29;500(7464):558-62. doi: 10.1038/nature12448.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Geology Department, University of Oviedo, Jesus Arias de Velasco S/N, 33005, Oviedo, Asturias, Spain. cbolton@geol.uniovi.es〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23985873" target="_blank"〉PubMed〈/a〉
    Keywords: Aquatic Organisms/*metabolism ; Atmosphere/chemistry ; Bicarbonates/metabolism ; Calcification, Physiologic ; Calcium Carbonate/chemistry/metabolism ; Carbon/metabolism ; Carbon Dioxide/analysis/*metabolism ; Carbon Isotopes ; Chloroplasts/metabolism ; Climate ; Fossils ; History, Ancient ; Oxygen Isotopes ; Partial Pressure ; Photosynthesis ; Phytoplankton/*metabolism ; Temperature
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  • 12
    Publication Date: 2014-02-21
    Description: The rapid increase of carbon dioxide concentration in Earth's modern atmosphere is a matter of major concern. But for the atmosphere of roughly two-and-half billion years ago, interest centres on a different gas: free oxygen (O2) spawned by early biological production. The initial increase of O2 in the atmosphere, its delayed build-up in the ocean, its increase to near-modern levels in the sea and air two billion years later, and its cause-and-effect relationship with life are among the most compelling stories in Earth's history.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Lyons, Timothy W -- Reinhard, Christopher T -- Planavsky, Noah J -- England -- Nature. 2014 Feb 20;506(7488):307-15. doi: 10.1038/nature13068.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth Sciences, University of California, Riverside, California 92521, USA. ; 1] Department of Earth Sciences, University of California, Riverside, California 92521, USA [2] Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA [3] School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 30332, USA. ; 1] Department of Earth Sciences, University of California, Riverside, California 92521, USA [2] Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06511, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24553238" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Atmosphere/*chemistry ; *Earth (Planet) ; *Evolution, Chemical ; History, Ancient ; Life ; Oxygen/analysis/history/*metabolism ; Photosynthesis ; Seawater/*chemistry
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  • 13
    Publication Date: 2014-04-25
    Description: Tropical forests are global epicentres of biodiversity and important modulators of climate change, and are mainly constrained by rainfall patterns. The severe short-term droughts that occurred recently in Amazonia have drawn attention to the vulnerability of tropical forests to climatic disturbances. The central African rainforests, the second-largest on Earth, have experienced a long-term drying trend whose impacts on vegetation dynamics remain mostly unknown because in situ observations are very limited. The Congolese forest, with its drier conditions and higher percentage of semi-evergreen trees, may be more tolerant to short-term rainfall reduction than are wetter tropical forests, but for a long-term drought there may be critical thresholds of water availability below which higher-biomass, closed-canopy forests transition to more open, lower-biomass forests. Here we present observational evidence for a widespread decline in forest greenness over the past decade based on analyses of satellite data (optical, thermal, microwave and gravity) from several independent sensors over the Congo basin. This decline in vegetation greenness, particularly in the northern Congolese forest, is generally consistent with decreases in rainfall, terrestrial water storage, water content in aboveground woody and leaf biomass, and the canopy backscatter anomaly caused by changes in structure and moisture in upper forest layers. It is also consistent with increases in photosynthetically active radiation and land surface temperature. These multiple lines of evidence indicate that this large-scale vegetation browning, or loss of photosynthetic capacity, may be partially attributable to the long-term drying trend. Our results suggest that a continued gradual decline of photosynthetic capacity and moisture content driven by the persistent drying trend could alter the composition and structure of the Congolese forest to favour the spread of drought-tolerant species.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Zhou, Liming -- Tian, Yuhong -- Myneni, Ranga B -- Ciais, Philippe -- Saatchi, Sassan -- Liu, Yi Y -- Piao, Shilong -- Chen, Haishan -- Vermote, Eric F -- Song, Conghe -- Hwang, Taehee -- England -- Nature. 2014 May 1;509(7498):86-90. doi: 10.1038/nature13265. Epub 2014 Apr 23.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York (SUNY), Albany, New York 12222, USA. ; I. M. Systems Group (IMSG), National Oceanic and Atmospheric Administration/National Environmental Satellite, Data, and Information Service/The Center for Satellite Applications and Research (NOAA/NESDIS/STAR), 5830 University Research Court, College Park, Maryland 20740, USA. ; Department of Earth and Environment, Boston University, Boston, Massachusetts 02215, USA. ; Laboratoire des Sciences du Climat et de l'Environnement (LSCE), CEA-CNRS-UVSQ, 91191 Gif sur Yvette Cedex, France. ; Jet Propulsion Laboratory, Pasadena, California 91109, USA. ; ARC Centre of Excellence for Climate Systems Science & Climate Change Research Centre, University of New South Wales, Sydney, New South Wales 2052, Australia. ; Department of Ecology, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China. ; Key Laboratory of Meteorological Disaster, Ministry of Education, Nanjing University of Information Science and Technology, Nanjing 210044, China. ; NASA Goddard Space Flight Center, Code 619, Greenbelt, Maryland 20771, USA. ; 1] Department of Geography, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 29599, USA [2] School of Forestry and Landscape Architecture, Anhui Agricultural University, Hefei, Anhui 230036, China. ; Institute for the Environment, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 29599, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24759324" target="_blank"〉PubMed〈/a〉
    Keywords: Acclimatization ; Biodiversity ; Biomass ; Chlorophyll/analysis/metabolism ; Climate Change/*statistics & numerical data ; Congo ; Droughts/statistics & numerical data ; Photosynthesis ; Plant Leaves/*growth & development/metabolism ; *Rain ; Satellite Imagery ; Seasons ; Temperature ; Time Factors ; Trees/*growth & development/metabolism ; *Tropical Climate ; Water/analysis/metabolism ; Wood/growth & development/metabolism
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  • 14
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    Nature Publishing Group (NPG)
    Publication Date: 2011-08-05
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Hutchins, David A -- England -- Nature. 2011 Aug 3;476(7358):41-2. doi: 10.1038/476041a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21814273" target="_blank"〉PubMed〈/a〉
    Keywords: Aquatic Organisms/chemistry/metabolism ; Atmosphere/chemistry ; *Calcification, Physiologic ; Calcium Carbonate/*analysis/chemistry/metabolism ; Carbon Cycle ; Carbon Dioxide/*analysis/chemistry ; Carbonic Acid/*analysis/chemistry ; Fossils ; Hydrogen-Ion Concentration ; Oceans and Seas ; Photosynthesis ; Phytoplankton/chemistry/*metabolism ; *Rain ; Seawater/*chemistry
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  • 15
    Publication Date: 2011-08-05
    Description: About one-third of the carbon dioxide (CO(2)) released into the atmosphere as a result of human activity has been absorbed by the oceans, where it partitions into the constituent ions of carbonic acid. This leads to ocean acidification, one of the major threats to marine ecosystems and particularly to calcifying organisms such as corals, foraminifera and coccolithophores. Coccolithophores are abundant phytoplankton that are responsible for a large part of modern oceanic carbonate production. Culture experiments investigating the physiological response of coccolithophore calcification to increased CO(2) have yielded contradictory results between and even within species. Here we quantified the calcite mass of dominant coccolithophores in the present ocean and over the past forty thousand years, and found a marked pattern of decreasing calcification with increasing partial pressure of CO(2) and concomitant decreasing concentrations of CO(3)(2-). Our analyses revealed that differentially calcified species and morphotypes are distributed in the ocean according to carbonate chemistry. A substantial impact on the marine carbon cycle might be expected upon extrapolation of this correlation to predicted ocean acidification in the future. However, our discovery of a heavily calcified Emiliania huxleyi morphotype in modern waters with low pH highlights the complexity of assemblage-level responses to environmental forcing factors.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Beaufort, L -- Probert, I -- de Garidel-Thoron, T -- Bendif, E M -- Ruiz-Pino, D -- Metzl, N -- Goyet, C -- Buchet, N -- Coupel, P -- Grelaud, M -- Rost, B -- Rickaby, R E M -- de Vargas, C -- 205150/European Research Council/International -- England -- Nature. 2011 Aug 3;476(7358):80-3. doi: 10.1038/nature10295.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉CEREGE, CNRS/Universite Aix-Marseille, Avenue L. Philibert BP80, 13545 Aix-en-Provence, Cedex 4, France. beaufort@cerege.fr〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21814280" target="_blank"〉PubMed〈/a〉
    Keywords: Aquatic Organisms/chemistry/metabolism ; Atmosphere/chemistry ; Body Weight ; *Calcification, Physiologic ; Calcium/metabolism ; Calcium Carbonate/*analysis/chemistry/metabolism ; Carbon Cycle ; Carbon Dioxide/analysis/chemistry ; Carbonic Acid/*analysis/chemistry ; Fossils ; Geologic Sediments/chemistry ; Haptophyta/chemistry/*metabolism ; Hydrogen-Ion Concentration ; Molecular Sequence Data ; Oceans and Seas ; Pacific Ocean ; Partial Pressure ; Photosynthesis ; Phytoplankton/chemistry/*metabolism ; Seawater/*chemistry
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  • 16
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    Unknown
    Nature Publishing Group (NPG)
    Publication Date: 2011-01-07
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉England -- Nature. 2011 Jan 6;469(7328):23-5. doi: 10.1038/469023a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21209640" target="_blank"〉PubMed〈/a〉
    Keywords: Biomimetics/trends ; Biopolymers/chemistry ; Chemistry/methods/*trends ; Conservation of Energy Resources/trends ; Drug Design ; Ecology/trends ; Global Warming ; Green Chemistry Technology/trends ; Molecular Biology/trends ; Nanotechnology/trends ; Photosynthesis ; Research Personnel ; Solar Energy ; Stereoisomerism ; Thermodynamics
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  • 17
    Publication Date: 2012-08-04
    Description: The warmest global climates of the past 65 million years occurred during the early Eocene epoch (about 55 to 48 million years ago), when the Equator-to-pole temperature gradients were much smaller than today and atmospheric carbon dioxide levels were in excess of one thousand parts per million by volume. Recently the early Eocene has received considerable interest because it may provide insight into the response of Earth's climate and biosphere to the high atmospheric carbon dioxide levels that are expected in the near future as a consequence of unabated anthropogenic carbon emissions. Climatic conditions of the early Eocene 'greenhouse world', however, are poorly constrained in critical regions, particularly Antarctica. Here we present a well-dated record of early Eocene climate on Antarctica from an ocean sediment core recovered off the Wilkes Land coast of East Antarctica. The information from biotic climate proxies (pollen and spores) and independent organic geochemical climate proxies (indices based on branched tetraether lipids) yields quantitative, seasonal temperature reconstructions for the early Eocene greenhouse world on Antarctica. We show that the climate in lowland settings along the Wilkes Land coast (at a palaeolatitude of about 70 degrees south) supported the growth of highly diverse, near-tropical forests characterized by mesothermal to megathermal floral elements including palms and Bombacoideae. Notably, winters were extremely mild (warmer than 10 degrees C) and essentially frost-free despite polar darkness, which provides a critical new constraint for the validation of climate models and for understanding the response of high-latitude terrestrial ecosystems to increased carbon dioxide forcing.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Pross, Jorg -- Contreras, Lineth -- Bijl, Peter K -- Greenwood, David R -- Bohaty, Steven M -- Schouten, Stefan -- Bendle, James A -- Rohl, Ursula -- Tauxe, Lisa -- Raine, J Ian -- Huck, Claire E -- van de Flierdt, Tina -- Jamieson, Stewart S R -- Stickley, Catherine E -- van de Schootbrugge, Bas -- Escutia, Carlota -- Brinkhuis, Henk -- Integrated Ocean Drilling Program Expedition 318 Scientists -- England -- Nature. 2012 Aug 2;488(7409):73-7. doi: 10.1038/nature11300.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Paleoenvironmental Dynamics Group, Institute of Geosciences, Goethe University Frankfurt, Altenhoferallee 1, 60438 Frankfurt, Germany. joerg.pross@em.uni-frankfurt.de〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22859204" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Antarctic Regions ; Atmosphere/chemistry ; Carbon Dioxide/analysis ; Cell Respiration ; Ecosystem ; Geologic Sediments/chemistry ; Greenhouse Effect/*history ; History, Ancient ; Human Activities ; Lipids/analysis ; Models, Theoretical ; Photosynthesis ; Pollen ; Reproducibility of Results ; Seasons ; Spores/isolation & purification ; *Temperature ; Trees/growth & development ; *Tropical Climate
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  • 18
    Publication Date: 2013-10-25
    Description: Globally, reef-building corals are the most prolific producers of dimethylsulphoniopropionate (DMSP), a central molecule in the marine sulphur cycle and precursor of the climate-active gas dimethylsulphide. At present, DMSP production by corals is attributed entirely to their algal endosymbiont, Symbiodinium. Combining chemical, genomic and molecular approaches, we show that coral juveniles produce DMSP in the absence of algal symbionts. DMSP levels increased up to 54% over time in newly settled coral juveniles lacking algal endosymbionts, and further increases, up to 76%, were recorded when juveniles were subjected to thermal stress. We uncovered coral orthologues of two algal genes recently identified in DMSP biosynthesis, strongly indicating that corals possess the enzymatic machinery necessary for DMSP production. Our results overturn the paradigm that photosynthetic organisms are the sole biological source of DMSP, and highlight the double jeopardy represented by worldwide declining coral cover, as the potential to alleviate thermal stress through coral-produced DMSP declines correspondingly.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Raina, Jean-Baptiste -- Tapiolas, Dianne M -- Foret, Sylvain -- Lutz, Adrian -- Abrego, David -- Ceh, Janja -- Seneca, Francois O -- Clode, Peta L -- Bourne, David G -- Willis, Bette L -- Motti, Cherie A -- England -- Nature. 2013 Oct 31;502(7473):677-80. doi: 10.1038/nature12677. Epub 2013 Oct 23.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉1] AIMS@JCU, and School of Marine and Tropical Biology, James Cook University, Townsville, Queensland 4811, Australia [2] Australian Institute of Marine Science, PMB3, Townsville MC, Townsville, Queensland 4810, Australia [3] ARC Centre of Excellence for Coral Reef Studies, School of Marine and Tropical Biology, James Cook University, Townsville, Queensland 4811, Australia.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24153189" target="_blank"〉PubMed〈/a〉
    Keywords: Acrylates/analysis/metabolism ; Algal Proteins/genetics ; Animals ; Anthozoa/genetics/metabolism/*physiology ; Climate Change ; Photosynthesis ; Secondary Metabolism ; *Stress, Physiological ; Sulfonium Compounds/*metabolism ; Symbiosis ; *Temperature ; Time Factors
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  • 19
    Publication Date: 2013-04-02
    Description: Meristems encompass stem/progenitor cells that sustain postembryonic growth of all plant organs. How meristems are activated and sustained by nutrient signalling remains enigmatic in photosynthetic plants. Combining chemical manipulations and chemical genetics at the photoautotrophic transition checkpoint, we reveal that shoot photosynthesis-derived glucose drives target-of-rapamycin (TOR) signalling relays through glycolysis and mitochondrial bioenergetics to control root meristem activation, which is decoupled from direct glucose sensing, growth-hormone signalling and stem-cell maintenance. Surprisingly, glucose-TOR signalling dictates transcriptional reprogramming of remarkable gene sets involved in central and secondary metabolism, cell cycle, transcription, signalling, transport and protein folding. Systems, cellular and genetic analyses uncover TOR phosphorylation of E2Fa transcription factor for an unconventional activation of S-phase genes, and glucose-signalling defects in e2fa root meristems. Our findings establish pivotal roles of glucose-TOR signalling in unprecedented transcriptional networks wiring central metabolism and biosynthesis for energy and biomass production, and integrating localized stem/progenitor-cell proliferation through inter-organ nutrient coordination to control developmental transition and growth.〈br /〉〈br /〉〈a href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4140196/" 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/PMC4140196/" target="_blank"〉This paper as free author manuscript - peer-reviewed and accepted for publication〈/a〉〈br /〉〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Xiong, Yan -- McCormack, Matthew -- Li, Lei -- Hall, Qi -- Xiang, Chengbin -- Sheen, Jen -- R01 GM060493/GM/NIGMS NIH HHS/ -- R01 GM070567/GM/NIGMS NIH HHS/ -- England -- Nature. 2013 Apr 11;496(7444):181-6. doi: 10.1038/nature12030. Epub 2013 Mar 31.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Molecular Biology and Centre for Computational and Integrative Biology, Massachusetts General Hospital, and Department of Genetics, Harvard Medical School, Boston, Massachusetts 02114, USA. xiong@molbio.mgh.harvard.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23542588" target="_blank"〉PubMed〈/a〉
    Keywords: Arabidopsis/*genetics/growth & development/*metabolism ; Arabidopsis Proteins/*metabolism ; Cytokinins/metabolism ; E2F Transcription Factors/metabolism ; Enzyme Activation ; *Gene Expression Regulation, Plant ; Gene Regulatory Networks/genetics ; Glucose/*metabolism ; Indoleacetic Acids/metabolism ; Meristem/genetics/growth & development/*metabolism ; Phosphatidylinositol 3-Kinases/*metabolism ; Phosphorylation ; Photosynthesis ; S Phase/genetics ; *Signal Transduction ; Transcription, Genetic/genetics ; Transcriptional Activation ; *Transcriptome/genetics
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  • 20
    Publication Date: 2013-04-13
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Schiermeier, Quirin -- England -- Nature. 2013 Apr 11;496(7444):147. doi: 10.1038/496147a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23579654" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; *Carbon Cycle ; Carbon Dioxide/*analysis/metabolism ; Carbon Sequestration ; Cell Respiration ; Congresses as Topic ; Droughts/statistics & numerical data ; Extreme Heat ; Feedback ; Greenhouse Effect/*statistics & numerical data ; Models, Theoretical ; Photosynthesis ; Plants/metabolism ; Soil Microbiology ; Water/metabolism ; *Weather
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  • 21
    Publication Date: 2013-09-27
    Description: It is widely assumed that atmospheric oxygen concentrations remained persistently low (less than 10(-5) times present levels) for about the first 2 billion years of Earth's history. The first long-term oxygenation of the atmosphere is thought to have taken place around 2.3 billion years ago, during the Great Oxidation Event. Geochemical indications of transient atmospheric oxygenation, however, date back to 2.6-2.7 billion years ago. Here we examine the distribution of chromium isotopes and redox-sensitive metals in the approximately 3-billion-year-old Nsuze palaeosol and in the near-contemporaneous Ijzermyn iron formation from the Pongola Supergroup, South Africa. We find extensive mobilization of redox-sensitive elements through oxidative weathering. Furthermore, using our data we compute a best minimum estimate for atmospheric oxygen concentrations at that time of 3 x 10(-4) times present levels. Overall, our findings suggest that there were appreciable levels of atmospheric oxygen about 3 billion years ago, more than 600 million years before the Great Oxidation Event and some 300-400 million years earlier than previous indications for Earth surface oxygenation.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Crowe, Sean A -- Dossing, Lasse N -- Beukes, Nicolas J -- Bau, Michael -- Kruger, Stephanus J -- Frei, Robert -- Canfield, Donald E -- England -- Nature. 2013 Sep 26;501(7468):535-8. doi: 10.1038/nature12426.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Institute of Biology, University of Southern Denmark, Odense 5230, Denmark. sean.crowe@ubc.ca〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24067713" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/*chemistry ; Biological Evolution ; Chromium Isotopes/analysis ; Cyanobacteria/metabolism ; Earth (Planet) ; Geologic Sediments/analysis/chemistry ; History, Ancient ; Iron/analysis ; Oxidation-Reduction ; Oxygen/*analysis/metabolism ; Photosynthesis ; South Africa
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  • 22
    Publication Date: 2014-02-07
    Description: The seasonality of sunlight and rainfall regulates net primary production in tropical forests. Previous studies have suggested that light is more limiting than water for tropical forest productivity, consistent with greening of Amazon forests during the dry season in satellite data. We evaluated four potential mechanisms for the seasonal green-up phenomenon, including increases in leaf area or leaf reflectance, using a sophisticated radiative transfer model and independent satellite observations from lidar and optical sensors. Here we show that the apparent green up of Amazon forests in optical remote sensing data resulted from seasonal changes in near-infrared reflectance, an artefact of variations in sun-sensor geometry. Correcting this bidirectional reflectance effect eliminated seasonal changes in surface reflectance, consistent with independent lidar observations and model simulations with unchanging canopy properties. The stability of Amazon forest structure and reflectance over seasonal timescales challenges the paradigm of light-limited net primary production in Amazon forests and enhanced forest growth during drought conditions. Correcting optical remote sensing data for artefacts of sun-sensor geometry is essential to isolate the response of global vegetation to seasonal and interannual climate variability.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Morton, Douglas C -- Nagol, Jyoteshwar -- Carabajal, Claudia C -- Rosette, Jacqueline -- Palace, Michael -- Cook, Bruce D -- Vermote, Eric F -- Harding, David J -- North, Peter R J -- England -- Nature. 2014 Feb 13;506(7487):221-4. doi: 10.1038/nature13006. Epub 2014 Feb 5.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉NASA Goddard Space Flight Center, Greenbelt, Maryland 20771, USA. ; 1] University of Maryland, College Park, Department of Geographical Sciences, College Park, Maryland 20742, USA [2] Global Land Cover Facility, College Park, Maryland 20740, USA. ; 1] NASA Goddard Space Flight Center, Greenbelt, Maryland 20771, USA [2] Sigma Space Corporation, Lantham, Maryland 20706, USA. ; 1] NASA Goddard Space Flight Center, Greenbelt, Maryland 20771, USA [2] University of Maryland, College Park, Department of Geographical Sciences, College Park, Maryland 20742, USA [3] Swansea University, Department of Geography, Singleton Park, Swansea SA2 8PP, UK. ; Earth System Research Center, University of New Hampshire, Durham, New Hampshire 03824, USA. ; Swansea University, Department of Geography, Singleton Park, Swansea SA2 8PP, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24499816" target="_blank"〉PubMed〈/a〉
    Keywords: Artifacts ; Brazil ; Color ; *Droughts ; Ecosystem ; Fresh Water/analysis ; Models, Biological ; Photosynthesis ; Pigmentation/*physiology ; Plant Leaves/anatomy & histology/growth & development/*physiology ; Rain ; Satellite Imagery ; *Seasons ; *Sunlight ; Trees/anatomy & histology/growth & development/*physiology ; *Tropical Climate
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  • 23
    facet.materialart.
    Unknown
    Nature Publishing Group (NPG)
    Publication Date: 2010-08-06
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Petherick, Anna -- England -- Nature. 2010 Aug 5;466(7307):675. doi: 10.1038/466675a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20686543" target="_blank"〉PubMed〈/a〉
    Keywords: Ambystoma/*embryology ; Animals ; Chlorophyta/*physiology ; Female ; Oviducts/metabolism ; Ovum/growth & development/*metabolism ; Photosynthesis ; *Symbiosis
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  • 24
    Publication Date: 2011-08-26
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Mayfield, Stephen -- Wong, P K -- England -- Nature. 2011 Aug 24;476(7361):402-3. doi: 10.1038/476402a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21866147" target="_blank"〉PubMed〈/a〉
    Keywords: *Biocatalysis ; Biochemical Processes ; Bioengineering/*methods ; Biofuels/*supply & distribution ; Biomass ; *Catalysis ; Chemical Engineering/*methods ; Conservation of Energy Resources/*methods ; Lignin/chemistry/metabolism ; Photosynthesis ; Saccharum/chemistry/metabolism ; Temperature ; Zea mays/chemistry/metabolism
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  • 25
    Publication Date: 2012-06-23
    Description: Ecosystem respiration is the biotic conversion of organic carbon to carbon dioxide by all of the organisms in an ecosystem, including both consumers and primary producers. Respiration exhibits an exponential temperature dependence at the subcellular and individual levels, but at the ecosystem level respiration can be modified by many variables including community abundance and biomass, which vary substantially among ecosystems. Despite its importance for predicting the responses of the biosphere to climate change, it is as yet unknown whether the temperature dependence of ecosystem respiration varies systematically between aquatic and terrestrial environments. Here we use the largest database of respiratory measurements yet compiled to show that the sensitivity of ecosystem respiration to seasonal changes in temperature is remarkably similar for diverse environments encompassing lakes, rivers, estuaries, the open ocean and forested and non-forested terrestrial ecosystems, with an average activation energy similar to that of the respiratory complex (approximately 0.65 electronvolts (eV)). By contrast, annual ecosystem respiration shows a substantially greater temperature dependence across aquatic (approximately 0.65 eV) versus terrestrial ecosystems (approximately 0.32 eV) that span broad geographic gradients in temperature. Using a model derived from metabolic theory, these findings can be reconciled by similarities in the biochemical kinetics of metabolism at the subcellular level, and fundamental differences in the importance of other variables besides temperature-such as primary productivity and allochthonous carbon inputs-on the structure of aquatic and terrestrial biota at the community level.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Yvon-Durocher, Gabriel -- Caffrey, Jane M -- Cescatti, Alessandro -- Dossena, Matteo -- del Giorgio, Paul -- Gasol, Josep M -- Montoya, Jose M -- Pumpanen, Jukka -- Staehr, Peter A -- Trimmer, Mark -- Woodward, Guy -- Allen, Andrew P -- England -- Nature. 2012 Jul 26;487(7408):472-6. doi: 10.1038/nature11205.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉School of Biological & Chemical Sciences, Queen Mary University of London, London E1 4NS, UK. g.yvon-durocher@exeter.ac.uk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22722862" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Biomass ; Biota ; Carbon/*metabolism ; Carbon Dioxide/*metabolism ; Cell Respiration ; Data Collection ; *Ecosystem ; *Global Warming ; Humans ; Kinetics ; Lakes ; Marine Biology ; *Oxygen Consumption ; Photosynthesis ; Rivers ; Seasons ; Seawater ; *Temperature ; Time Factors ; Trees/metabolism
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  • 26
    Publication Date: 2013-04-05
    Description: Renewable fresh water over continents has input from precipitation and losses to the atmosphere through evaporation and transpiration. Global-scale estimates of transpiration from climate models are poorly constrained owing to large uncertainties in stomatal conductance and the lack of catchment-scale measurements required for model calibration, resulting in a range of predictions spanning 20 to 65 per cent of total terrestrial evapotranspiration (14,000 to 41,000 km(3) per year) (refs 1, 2, 3, 4, 5). Here we use the distinct isotope effects of transpiration and evaporation to show that transpiration is by far the largest water flux from Earth's continents, representing 80 to 90 per cent of terrestrial evapotranspiration. On the basis of our analysis of a global data set of large lakes and rivers, we conclude that transpiration recycles 62,000 +/- 8,000 km(3) of water per year to the atmosphere, using half of all solar energy absorbed by land surfaces in the process. We also calculate CO2 uptake by terrestrial vegetation by connecting transpiration losses to carbon assimilation using water-use efficiency ratios of plants, and show the global gross primary productivity to be 129 +/- 32 gigatonnes of carbon per year, which agrees, within the uncertainty, with previous estimates. The dominance of transpiration water fluxes in continental evapotranspiration suggests that, from the point of view of water resource forecasting, climate model development should prioritize improvements in simulations of biological fluxes rather than physical (evaporation) fluxes.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Jasechko, Scott -- Sharp, Zachary D -- Gibson, John J -- Birks, S Jean -- Yi, Yi -- Fawcett, Peter J -- England -- Nature. 2013 Apr 18;496(7445):347-50. doi: 10.1038/nature11983. Epub 2013 Apr 3.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA. jasechko@unm.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23552893" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/chemistry ; Carbon Dioxide/analysis/metabolism ; Ecosystem ; Fresh Water/*analysis/chemistry ; Lakes ; Oceans and Seas ; Photosynthesis ; Plant Transpiration/*physiology ; Plants/*metabolism ; Rain ; Rivers ; Uncertainty ; Volatilization ; *Water Movements
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  • 27
    Publication Date: 2013-03-08
    Description: Geological evidence suggests that marine ice extended to the Equator at least twice during the Neoproterozoic era (about 750 to 635 million years ago), inspiring the Snowball Earth hypothesis that the Earth was globally ice-covered. In a possible Snowball Earth climate, ocean circulation and mixing processes would have set the melting and freezing rates that determine ice thickness, would have influenced the survival of photosynthetic life, and may provide important constraints for the interpretation of geochemical and sedimentological observations. Here we show that in a Snowball Earth, the ocean would have been well mixed and characterized by a dynamic circulation, with vigorous equatorial meridional overturning circulation, zonal equatorial jets, a well developed eddy field, strong coastal upwelling and convective mixing. This is in contrast to the sluggish ocean often expected in a Snowball Earth scenario owing to the insulation of the ocean from atmospheric forcing by the thick ice cover. As a result of vigorous convective mixing, the ocean temperature, salinity and density were either uniform in the vertical direction or weakly stratified in a few locations. Our results are based on a model that couples ice flow and ocean circulation, and is driven by a weak geothermal heat flux under a global ice cover about a kilometre thick. Compared with the modern ocean, the Snowball Earth ocean had far larger vertical mixing rates, and comparable horizontal mixing by ocean eddies. The strong circulation and coastal upwelling resulted in melting rates near continents as much as ten times larger than previously estimated. Although we cannot resolve the debate over the existence of global ice cover, we discuss the implications for the nutrient supply of photosynthetic activity and for banded iron formations. Our insights and constraints on ocean dynamics may help resolve the Snowball Earth controversy when combined with future geochemical and geological observations.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Ashkenazy, Yosef -- Gildor, Hezi -- Losch, Martin -- Macdonald, Francis A -- Schrag, Daniel P -- Tziperman, Eli -- England -- Nature. 2013 Mar 7;495(7439):90-3. doi: 10.1038/nature11894.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Solar Energy and Environmental Physics, The Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Midreshet Ben-Gurion, 84990, Israel. ashkena@bgu.ac.il〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23467167" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; *Earth (Planet) ; History, Ancient ; *Ice Cover ; Models, Theoretical ; Oceans and Seas ; Photosynthesis ; Salinity ; *Seawater/analysis/chemistry ; *Snow ; Temperature ; *Water Movements
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 28
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    Nature Publishing Group (NPG)
    Publication Date: 2014-11-05
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Dayton, Leigh -- England -- Nature. 2014 Oct 30;514(7524):S52-4.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25368887" target="_blank"〉PubMed〈/a〉
    Keywords: Agriculture/*methods/trends ; Australia ; Biotechnology/*trends ; Crops, Agricultural/genetics/growth & development/microbiology/supply & ; distribution ; Fertilizers ; Food Supply ; Nitrogen/metabolism ; Oryza/*genetics/growth & development/microbiology/*supply & distribution ; Photosynthesis ; Plant Diseases/genetics/microbiology
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 29
    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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  • 30
    Publication Date: 2014-06-27
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Morello, Lauren -- England -- Nature. 2014 Jun 26;510(7506):451-2. doi: 10.1038/510451a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24965628" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/chemistry ; Carbon Dioxide/*analysis ; Environmental Monitoring/*instrumentation ; Fossil Fuels ; *Geographic Mapping ; *Greenhouse Effect ; Luminescent Measurements/instrumentation ; Photosynthesis ; Plants/metabolism ; Satellite Imagery/*instrumentation ; United States ; United States National Aeronautics and Space Administration
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    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 31
    Publication Date: 2014-02-07
    Description: Feedbacks between land carbon pools and climate provide one of the largest sources of uncertainty in our predictions of global climate. Estimates of the sensitivity of the terrestrial carbon budget to climate anomalies in the tropics and the identification of the mechanisms responsible for feedback effects remain uncertain. The Amazon basin stores a vast amount of carbon, and has experienced increasingly higher temperatures and more frequent floods and droughts over the past two decades. Here we report seasonal and annual carbon balances across the Amazon basin, based on carbon dioxide and carbon monoxide measurements for the anomalously dry and wet years 2010 and 2011, respectively. We find that the Amazon basin lost 0.48 +/- 0.18 petagrams of carbon per year (Pg C yr(-1)) during the dry year but was carbon neutral (0.06 +/- 0.1 Pg C yr(-1)) during the wet year. Taking into account carbon losses from fire by using carbon monoxide measurements, we derived the basin net biome exchange (that is, the carbon flux between the non-burned forest and the atmosphere) revealing that during the dry year, vegetation was carbon neutral. During the wet year, vegetation was a net carbon sink of 0.25 +/- 0.14 Pg C yr(-1), which is roughly consistent with the mean long-term intact-forest biomass sink of 0.39 +/- 0.10 Pg C yr(-1) previously estimated from forest censuses. Observations from Amazonian forest plots suggest the suppression of photosynthesis during drought as the primary cause for the 2010 sink neutralization. Overall, our results suggest that moisture has an important role in determining the Amazonian carbon balance. If the recent trend of increasing precipitation extremes persists, the Amazon may become an increasing carbon source as a result of both emissions from fires and the suppression of net biome exchange by drought.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Gatti, L V -- Gloor, M -- Miller, J B -- Doughty, C E -- Malhi, Y -- Domingues, L G -- Basso, L S -- Martinewski, A -- Correia, C S C -- Borges, V F -- Freitas, S -- Braz, R -- Anderson, L O -- Rocha, H -- Grace, J -- Phillips, O L -- Lloyd, J -- England -- Nature. 2014 Feb 6;506(7486):76-80. doi: 10.1038/nature12957.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉1] Instituto de Pesquisas Energeticas e Nucleares (IPEN)-Comissao Nacional de Energia Nuclear (CNEN)-Atmospheric Chemistry Laboratory, 2242 Avenida Professor Lineu Prestes, Cidade Universitaria, Sao Paulo CEP 05508-000, Brazil [2]. ; 1] School of Geography, University of Leeds, Woodhouse Lane, Leeds LS9 2JT, UK [2]. ; 1] Global Monitoring Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration, 325 Broadway, Boulder, Colorado 80305, USA [2] Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, Colorado 80309, USA [3]. ; Environmental Change Institute, School of Geography and the Environment, University of Oxford, South Parks Road, Oxford OX1 3QY, UK. ; Instituto de Pesquisas Energeticas e Nucleares (IPEN)-Comissao Nacional de Energia Nuclear (CNEN)-Atmospheric Chemistry Laboratory, 2242 Avenida Professor Lineu Prestes, Cidade Universitaria, Sao Paulo CEP 05508-000, Brazil. ; Center for Weather Forecasts and Climate Studies, Instituto Nacional de Pesquisas Espaciais (INPE), Rodovia Dutra, km 39, Cachoeira Paulista CEP 12630-000, Brazil. ; 1] Environmental Change Institute, School of Geography and the Environment, University of Oxford, South Parks Road, Oxford OX1 3QY, UK [2] Remote Sensing Division, INPE (National Institute for Space Research), 1758 Avenida dos Astronautas, Sao Jose dos Campos CEP 12227-010, Brazil. ; Departamento de Ciencias Atmosfericas/Instituto de Astronomia e Geofisica (IAG)/Universidade de Sao Paulo, 1226 Rua do Matao, Cidade Universitaria, Sao Paulo CEP 05508-090, Brazil. ; Crew Building, The King's Buildings, West Mains Road, Edinburgh EH9 3JN, UK. ; School of Geography, University of Leeds, Woodhouse Lane, Leeds LS9 2JT, UK. ; 1] School of Tropical and Marine Biology and Centre for Terrestrial Environmental and Sustainability Sciences, James Cook University, Cairns 4870, Queensland, Australia [2] Imperial College London, Silwood Park Campus, Buckhurst Road, Ascot SL5 7PY, Berkshire, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24499918" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/*chemistry ; Biomass ; Biota ; Brazil ; *Carbon Cycle ; Carbon Dioxide/analysis ; Carbon Monoxide/analysis ; Droughts/*statistics & numerical data ; Fires/statistics & numerical data ; Fresh Water/analysis ; Photosynthesis ; Rain ; Seasons ; Trees/metabolism ; Tropical Climate
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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