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  • Climate
  • Nature Publishing Group (NPG)  (23)
  • Annual Reviews  (1)
  • American Chemical Society
  • American Physical Society
  • 2015-2019  (12)
  • 2005-2009  (12)
  • 1980-1984
  • 1
    Publication Date: 2008-08-30
    Description: It is thought that the Northern Hemisphere experienced only ephemeral glaciations from the Late Eocene to the Early Pliocene epochs (about 38 to 4 million years ago), and that the onset of extensive glaciations did not occur until about 3 million years ago. Several hypotheses have been proposed to explain this increase in Northern Hemisphere glaciation during the Late Pliocene. Here we use a fully coupled atmosphere-ocean general circulation model and an ice-sheet model to assess the impact of the proposed driving mechanisms for glaciation and the influence of orbital variations on the development of the Greenland ice sheet in particular. We find that Greenland glaciation is mainly controlled by a decrease in atmospheric carbon dioxide during the Late Pliocene. By contrast, our model results suggest that climatic shifts associated with the tectonically driven closure of the Panama seaway, with the termination of a permanent El Nino state or with tectonic uplift are not large enough to contribute significantly to the growth of the Greenland ice sheet; moreover, we find that none of these processes acted as a priming mechanism for glacial inception triggered by variations in the Earth's orbit.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Lunt, Daniel J -- Foster, Gavin L -- Haywood, Alan M -- Stone, Emma J -- England -- Nature. 2008 Aug 28;454(7208):1102-5. doi: 10.1038/nature07223.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉BRIDGE, School of Geographical Sciences, University of Bristol, University Road, Bristol BS8 1SS, UK. d.j.lunt@bristol.ac.uk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18756254" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/*chemistry ; Carbon Dioxide/analysis/*metabolism ; Climate ; Greenland ; History, Ancient ; *Ice Cover ; North America ; Rain ; Time Factors
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    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 2
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    Nature Publishing Group (NPG)
    Publication Date: 2008-12-19
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Billings, Sharon A -- England -- Nature. 2008 Dec 18;456(7224):888-9. doi: 10.1038/456888a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19092923" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/chemistry ; Climate ; Droughts ; Europe ; Humidity ; Nitrous Oxide/*metabolism ; Picea/metabolism ; Rain ; Soil/*analysis ; Trees/*metabolism
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  • 3
    Publication Date: 2008-09-12
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Butler, Declan -- England -- Nature. 2008 Sep 11;455(7210):142-3. doi: 10.1038/455142b.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18784680" target="_blank"〉PubMed〈/a〉
    Keywords: Air Pollution/*statistics & numerical data ; Cities/*statistics & numerical data ; City Planning/trends ; Climate ; Data Collection/economics ; Databases, Factual ; Europe ; Models, Theoretical ; Population Density
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  • 4
    Publication Date: 2009-02-06
    Description: The Atlantic meridional overturning circulation (AMOC) transports warm salty surface waters to high latitudes, where they cool, sink and return southwards at depth. Through its attendant meridional heat transport, the AMOC helps maintain a warm northwestern European climate, and acts as a control on the global climate. Past climate fluctuations during the Holocene epoch ( approximately 11,700 years ago to the present) have been linked with changes in North Atlantic Ocean circulation. The behaviour of the surface flowing salty water that helped drive overturning during past climatic changes is, however, not well known. Here we investigate the temperature and salinity changes of a substantial surface inflow to a region of deep-water formation throughout the Holocene. We find that the inflow has undergone millennial-scale variations in temperature and salinity ( approximately 3.5 degrees C and approximately 1.5 practical salinity units, respectively) most probably controlled by subpolar gyre dynamics. The temperature and salinity variations correlate with previously reported periods of rapid climate change. The inflow becomes more saline during enhanced freshwater flux to the subpolar North Atlantic. Model studies predict a weakening of AMOC in response to enhanced Arctic freshwater fluxes, although the inflow can compensate on decadal timescales by becoming more saline. Our data suggest that such a negative feedback mechanism may have operated during past intervals of climate change.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Thornalley, David J R -- Elderfield, Harry -- McCave, I Nick -- England -- Nature. 2009 Feb 5;457(7230):711-4. doi: 10.1038/nature07717.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉The Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK. d.thornalley@cantab.net〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19194447" target="_blank"〉PubMed〈/a〉
    Keywords: Atlantic Ocean ; Calcium Carbonate/analysis ; Climate ; Feedback ; Fresh Water/analysis/chemistry ; History, Ancient ; Oxygen Isotopes ; Plankton/metabolism ; *Salinity ; Seawater/*chemistry ; *Temperature ; *Water Movements
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  • 5
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    Nature Publishing Group (NPG)
    Publication Date: 2009-09-26
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Diamond, Jared -- England -- Nature. 2009 Sep 24;461(7263):479-80. doi: 10.1038/461479a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19779438" target="_blank"〉PubMed〈/a〉
    Keywords: Agriculture/history ; Animals ; Archaeology ; Cambodia ; Central America ; Civilization/*history ; Climate ; Droughts ; Forestry/*history ; History, 15th Century ; History, 16th Century ; History, 17th Century ; History, Medieval ; Population Density ; South America ; Trees/growth & development ; Wood/history
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  • 6
    Publication Date: 2009-09-04
    Description: Complex dynamical systems, ranging from ecosystems to financial markets and the climate, can have tipping points at which a sudden shift to a contrasting dynamical regime may occur. Although predicting such critical points before they are reached is extremely difficult, work in different scientific fields is now suggesting the existence of generic early-warning signals that may indicate for a wide class of systems if a critical threshold is approaching.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Scheffer, Marten -- Bascompte, Jordi -- Brock, William A -- Brovkin, Victor -- Carpenter, Stephen R -- Dakos, Vasilis -- Held, Hermann -- van Nes, Egbert H -- Rietkerk, Max -- Sugihara, George -- England -- Nature. 2009 Sep 3;461(7260):53-9. doi: 10.1038/nature08227.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Environmental Sciences, Wageningen University, PO Box 47, 6700 AA Wageningen, The Netherlands. marten.scheffer@wur.nl〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19727193" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Asthma/physiopathology ; Climate ; *Ecosystem ; Eutrophication ; Extinction, Biological ; Humans ; *Models, Biological ; *Models, Economic ; Seizures/physiopathology ; Stochastic Processes
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  • 7
    Publication Date: 2009-09-26
    Description: Reconstructions of atmospheric CO(2) concentrations based on Antarctic ice cores reveal significant changes during the Holocene epoch, but the processes responsible for these changes in CO(2) concentrations have not been unambiguously identified. Distinct characteristics in the carbon isotope signatures of the major carbon reservoirs (ocean, biosphere, sediments and atmosphere) constrain variations in the CO(2) fluxes between those reservoirs. Here we present a highly resolved atmospheric delta(13)C record for the past 11,000 years from measurements on atmospheric CO(2) trapped in an Antarctic ice core. From mass-balance inverse model calculations performed with a simplified carbon cycle model, we show that the decrease in atmospheric CO(2) of about 5 parts per million by volume (p.p.m.v.). The increase in delta(13)C of about 0.25 per thousand during the early Holocene is most probably the result of a combination of carbon uptake of about 290 gigatonnes of carbon by the land biosphere and carbon release from the ocean in response to carbonate compensation of the terrestrial uptake during the termination of the last ice age. The 20 p.p.m.v. increase of atmospheric CO(2) and the small decrease in delta(13)C of about 0.05 per thousand during the later Holocene can mostly be explained by contributions from carbonate compensation of earlier land-biosphere uptake and coral reef formation, with only a minor contribution from a small decrease of the land-biosphere carbon inventory.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Elsig, Joachim -- Schmitt, Jochen -- Leuenberger, Daiana -- Schneider, Robert -- Eyer, Marc -- Leuenberger, Markus -- Joos, Fortunat -- Fischer, Hubertus -- Stocker, Thomas F -- England -- Nature. 2009 Sep 24;461(7263):507-10. doi: 10.1038/nature08393.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19779448" target="_blank"〉PubMed〈/a〉
    Keywords: Air/analysis ; Animals ; Antarctic Regions ; Anthozoa/growth & development/metabolism ; Atmosphere/chemistry ; Carbon/*analysis/*metabolism ; Carbon Dioxide/analysis/*metabolism ; Carbon Isotopes ; Climate ; Ecosystem ; History, Ancient ; Ice Cover/*chemistry ; Time Factors
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  • 8
    Publication Date: 2009-08-08
    Description: The detection of methane on Mars has revived the possibility of past or extant life on this planet, despite the fact that an abiogenic origin is thought to be equally plausible. An intriguing aspect of the recent observations of methane on Mars is that methane concentrations appear to be locally enhanced and change with the seasons. However, methane has a photochemical lifetime of several centuries, and is therefore expected to have a spatially uniform distribution on the planet. Here we use a global climate model of Mars with coupled chemistry to examine the implications of the recently observed variations of Martian methane for our understanding of the chemistry of methane. We find that photochemistry as currently understood does not produce measurable variations in methane concentrations, even in the case of a current, local and episodic methane release. In contrast, we find that the condensation-sublimation cycle of Mars' carbon dioxide atmosphere can generate large-scale methane variations differing from those observed. In order to reproduce local methane enhancements similar to those recently reported, we show that an atmospheric lifetime of less than 200 days is necessary, even if a local source of methane is only active around the time of the observation itself. This implies an unidentified methane loss process that is 600 times faster than predicted by standard photochemistry. The existence of such a fast loss in the Martian atmosphere is difficult to reconcile with the observed distribution of other trace gas species. In the case of a destruction mechanism only active at the surface of Mars, destruction of methane must occur with an even shorter timescale of the order of approximately 1 hour to explain the observations. If recent observations of spatial and temporal variations of methane are confirmed, this would suggest an extraordinarily harsh environment for the survival of organics on the planet.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Lefevre, Franck -- Forget, Francois -- England -- Nature. 2009 Aug 6;460(7256):720-3. doi: 10.1038/nature08228.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉LATMOS, UPMC Universite Paris 06, CNRS, Paris 75005, France. franck.lefevre@upmc.fr〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19661912" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/chemistry ; Carbon Dioxide/analysis ; Climate ; Electrochemistry ; Exobiology ; Extraterrestrial Environment/*chemistry ; *Mars ; Methane/*analysis ; Models, Chemical ; Photochemistry ; Time Factors
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  • 9
    Publication Date: 2009-07-03
    Description: Environmental conditions during the past 24 million years are thought to have been favourable for enhanced rates of atmospheric carbon dioxide drawdown by silicate chemical weathering. Proxy records indicate, however, that the Earth's atmospheric carbon dioxide concentrations did not fall below about 200-250 parts per million during this period. The stabilization of atmospheric carbon dioxide concentrations near this minimum value suggests that strong negative feedback mechanisms inhibited further drawdown of atmospheric carbon dioxide by high rates of global silicate rock weathering. Here we investigate one possible negative feedback mechanism, occurring under relatively low carbon dioxide concentrations and in warm climates, that is related to terrestrial plant productivity and its role in the decomposition of silicate minerals. We use simulations of terrestrial and geochemical carbon cycles and available experimental evidence to show that vegetation activity in upland regions of active orogens was severely limited by near-starvation of carbon dioxide in combination with global warmth over this period. These conditions diminished biotic-driven silicate rock weathering and thereby attenuated an important long-term carbon dioxide sink. Although our modelling results are semi-quantitative and do not capture the full range of biogeochemical feedbacks that could influence the climate, our analysis indicates that the dynamic equilibrium between plants, climate and the geosphere probably buffered the minimum atmospheric carbon dioxide concentrations over the past 24 million years.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Pagani, Mark -- Caldeira, Ken -- Berner, Robert -- Beerling, David J -- England -- Nature. 2009 Jul 2;460(7251):85-8. doi: 10.1038/nature08133.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06520, USA. mark.pagani@yale.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19571882" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Atmosphere/*chemistry ; Biomass ; Carbon Dioxide/*analysis ; Climate ; Eukaryota ; Geologic Sediments/*chemistry ; Geology ; History, Ancient ; Ice Cover ; Models, Biological ; Plant Leaves/metabolism ; Plant Roots/growth & development ; Plant Transpiration ; Plants/*metabolism ; Silicates/*chemistry
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  • 10
    Publication Date: 2009-10-09
    Description: Relative to the present day, meridional temperature gradients in the Early Eocene age ( approximately 56-53 Myr ago) were unusually low, with slightly warmer equatorial regions but with much warmer subtropical Arctic and mid-latitude climates. By the end of the Eocene epoch ( approximately 34 Myr ago), the first major Antarctic ice sheets had appeared, suggesting that major cooling had taken place. Yet the global transition into this icehouse climate remains poorly constrained, as only a few temperature records are available portraying the Cenozoic climatic evolution of the high southern latitudes. Here we present a uniquely continuous and chronostratigraphically well-calibrated TEX(86) record of sea surface temperature (SST) from an ocean sediment core in the East Tasman Plateau (palaeolatitude approximately 65 degrees S). We show that southwest Pacific SSTs rose above present-day tropical values (to approximately 34 degrees C) during the Early Eocene age ( approximately 53 Myr ago) and had gradually decreased to about 21 degrees C by the early Late Eocene age ( approximately 36 Myr ago). Our results imply that there was almost no latitudinal SST gradient between subequatorial and subpolar regions during the Early Eocene age (55-50 Myr ago). Thereafter, the latitudinal gradient markedly increased. In theory, if Eocene cooling was largely driven by a decrease in atmospheric greenhouse gas concentration, additional processes are required to explain the relative stability of tropical SSTs given that there was more significant cooling at higher latitudes.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Bijl, Peter K -- Schouten, Stefan -- Sluijs, Appy -- Reichart, Gert-Jan -- Zachos, James C -- Brinkhuis, Henk -- England -- Nature. 2009 Oct 8;461(7265):776-9. doi: 10.1038/nature08399.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Palaeoecology, Institute of Environmental Biology, Faculty of Science, Laboratory of Palaeobotany and Palynology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands. p.k.bijl@uu.nl〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19812670" target="_blank"〉PubMed〈/a〉
    Keywords: Antarctic Regions ; Biological Evolution ; Climate ; Geologic Sediments/analysis/chemistry ; History, Ancient ; Ice Cover ; Oxygen Isotopes ; Pacific Ocean ; Plankton/metabolism ; Seawater/*analysis ; *Temperature ; Water Movements
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  • 11
    Publication Date: 2009-07-03
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Godderis, Yves -- Donnadieu, Yannick -- England -- Nature. 2009 Jul 2;460(7251):40-1. doi: 10.1038/460040a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19571871" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Atmosphere/*chemistry ; Carbon Dioxide/*analysis/chemistry ; Climate ; Geologic Sediments/*chemistry ; History, Ancient ; Plants/*metabolism
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  • 12
    Publication Date: 2015-08-01
    Description: Earth's mightiest ocean current, the Antarctic Circumpolar Current (ACC), regulates the exchange of heat and carbon between the ocean and the atmosphere, and influences vertical ocean structure, deep-water production and the global distribution of nutrients and chemical tracers. The eastward-flowing ACC occupies a unique circumglobal pathway in the Southern Ocean that was enabled by the tectonic opening of key oceanic gateways during the break-up of Gondwana (for example, by the opening of the Tasmanian Gateway, which connects the Indian and Pacific oceans). Although the ACC is a key component of Earth's present and past climate system, the timing of the appearance of diagnostic features of the ACC (for example, low zonal gradients in water-mass tracer fields) is poorly known and represents a fundamental gap in our understanding of Earth history. Here we show, using geophysically determined positions of continent-ocean boundaries, that the deep Tasmanian Gateway opened 33.5 +/- 1.5 million years ago (the errors indicate uncertainty in the boundary positions). Following this opening, sediments from Indian and Pacific cores recorded Pacific-type neodymium isotope ratios, revealing deep westward flow equivalent to the present-day Antarctic Slope Current. We observe onset of the ACC at around 30 million years ago, when Southern Ocean neodymium isotopes record a permanent shift to modern Indian-Atlantic ratios. Our reconstructions of ocean circulation show that massive reorganization and homogenization of Southern Ocean water masses coincided with migration of the northern margin of the Tasmanian Gateway into the mid-latitude westerly wind band, which we reconstruct at 64 degrees S, near to the northern margin. Onset of the ACC about 30 million years ago coincided with major changes in global ocean circulation and probably contributed to the lower atmospheric carbon dioxide levels that appear after this time.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Scher, Howie D -- Whittaker, Joanne M -- Williams, Simon E -- Latimer, Jennifer C -- Kordesch, Wendy E C -- Delaney, Margaret L -- England -- Nature. 2015 Jul 30;523(7562):580-3. doi: 10.1038/nature14598.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth and Ocean Sciences, University of South Carolina, Columbia, South Carolina 29208, USA. ; Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Tasmania 7001, Australia. ; EarthByte group, School of Geosciences, The University of Sydney, Sydney, New South Wales 2006, Australia. ; Department of Earth and Environmental Systems, Indiana State University, Terre Haute, Indiana 47809, USA. ; Department of Ocean and Earth Science, National Oceanography Centre, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK. ; Ocean Sciences Department and Institute of Marine Sciences, University of California Santa Cruz, Santa Cruz, California 95064, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26223626" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Antarctic Regions ; Atmosphere/chemistry ; Carbon/analysis ; Carbon Dioxide/analysis ; Climate ; Fishes ; Fossils ; Geologic Sediments/chemistry ; History, Ancient ; Hot Temperature ; Isotopes ; Neodymium/analysis ; Oceans and Seas ; Seawater/analysis/chemistry ; Tooth ; *Water Movements ; *Wind
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  • 13
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    Nature Publishing Group (NPG)
    Publication Date: 2015-01-17
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Zastrow, Mark -- England -- Nature. 2015 Jan 15;517(7534):256-7. doi: 10.1038/517256a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25592515" target="_blank"〉PubMed〈/a〉
    Keywords: Climate ; *Earth (Planet) ; Environmental Monitoring/*instrumentation ; Environmental Pollution/analysis ; Extraterrestrial Environment/chemistry ; Models, Theoretical ; Politics ; Seasons ; *Spacecraft ; United States ; United States National Aeronautics and Space Administration
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  • 14
    Publication Date: 2015-06-13
    Description: Our current understanding of ocean-atmosphere-cryosphere interactions at ice-age terminations relies largely on assessments of the most recent (last) glacial-interglacial transition, Termination I (T-I). But the extent to which T-I is representative of previous terminations remains unclear. Testing the consistency of termination processes requires comparison of time series of critical climate parameters with detailed absolute and relative age control. However, such age control has been lacking for even the penultimate glacial termination (T-II), which culminated in a sea-level highstand during the last interglacial period that was several metres above present. Here we show that Heinrich Stadial 11 (HS11), a prominent North Atlantic cold episode, occurred between 135 +/- 1 and 130 +/- 2 thousand years ago and was linked with rapid sea-level rise during T-II. Our conclusions are based on new and existing data for T-II and the last interglacial that we collate onto a single, radiometrically constrained chronology. The HS11 cold episode punctuated T-II and coincided directly with a major deglacial meltwater pulse, which predominantly entered the North Atlantic Ocean and accounted for about 70 per cent of the glacial-interglacial sea-level rise. We conclude that, possibly in response to stronger insolation and CO2 forcing earlier in T-II, the relationship between climate and ice-volume changes differed fundamentally from that of T-I. In T-I, the major sea-level rise clearly post-dates Heinrich Stadial 1. We also find that HS11 coincided with sustained Antarctic warming, probably through a bipolar seesaw temperature response, and propose that this heat gain at high southern latitudes promoted Antarctic ice-sheet melting that fuelled the last interglacial sea-level peak.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Marino, G -- Rohling, E J -- Rodriguez-Sanz, L -- Grant, K M -- Heslop, D -- Roberts, A P -- Stanford, J D -- Yu, J -- England -- Nature. 2015 Jun 11;522(7555):197-201. doi: 10.1038/nature14499.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Research School of Earth Sciences, The Australian National University, Canberra, Australian Capital Territory 2601, Australia. ; 1] Research School of Earth Sciences, The Australian National University, Canberra, Australian Capital Territory 2601, Australia [2] Ocean and Earth Science, University of Southampton, National Oceanography Centre, Southampton SO14 3ZH, UK. ; Department of Geography, Wallace Building, Swansea University, Singleton Park, Swansea SA2 8PP, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26062511" target="_blank"〉PubMed〈/a〉
    Keywords: Antarctic Regions ; Aquatic Organisms/metabolism ; Atlantic Ocean ; Climate ; Foraminifera/metabolism ; History, Ancient ; *Ice Cover ; Mediterranean Region ; Mediterranean Sea ; Plankton/metabolism ; Seawater/*analysis ; Temperature
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  • 15
    Publication Date: 2015-02-13
    Description: Atmospheric CO2 fluctuations over glacial-interglacial cycles remain a major challenge to our understanding of the carbon cycle and the climate system. Leading hypotheses put forward to explain glacial-interglacial atmospheric CO2 variations invoke changes in deep-ocean carbon storage, probably modulated by processes in the Southern Ocean, where much of the deep ocean is ventilated. A central aspect of such models is that, during deglaciations, an isolated glacial deep-ocean carbon reservoir is reconnected with the atmosphere, driving the atmospheric CO2 rise observed in ice-core records. However, direct documentation of changes in surface ocean carbon content and the associated transfer of carbon to the atmosphere during deglaciations has been hindered by the lack of proxy reconstructions that unambiguously reflect the oceanic carbonate system. Radiocarbon activity tracks changes in ocean ventilation, but not in ocean carbon content, whereas proxies that record increased deglacial upwelling do not constrain the proportion of upwelled carbon that is degassed relative to that which is taken up by the biological pump. Here we apply the boron isotope pH proxy in planktic foraminifera to two sediment cores from the sub-Antarctic Atlantic and the eastern equatorial Pacific as a more direct tracer of oceanic CO2 outgassing. We show that surface waters at both locations, which partly derive from deep water upwelled in the Southern Ocean, became a significant source of carbon to the atmosphere during the last deglaciation, when the concentration of atmospheric CO2 was increasing. This oceanic CO2 outgassing supports the view that the ventilation of a deep-ocean carbon reservoir in the Southern Ocean had a key role in the deglacial CO2 rise, although our results allow for the possibility that processes operating in other regions may also have been important for the glacial-interglacial ocean-atmosphere exchange of carbon.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Martinez-Boti, M A -- Marino, G -- Foster, G L -- Ziveri, P -- Henehan, M J -- Rae, J W B -- Mortyn, P G -- Vance, D -- England -- Nature. 2015 Feb 12;518(7538):219-22. doi: 10.1038/nature14155.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus, Southampton SO14 3ZH, UK. ; 1] Institute of Environmental Science and Technology (ICTA), Universitat Autonoma de Barcelona, Bellaterra, Catalonia, 08193, Spain [2] Research School of Earth Sciences, The Australian National University, Canberra, Australian Capital Territory 2601, Australia. ; 1] Institute of Environmental Science and Technology (ICTA), Universitat Autonoma de Barcelona, Bellaterra, Catalonia, 08193, Spain [2] Institucio Catalana de Recerca i Estudis Avancats, ICREA, Barcelona, Catalonia, 08010, Spain [3] Earth and Climate Cluster, Department of Earth Sciences, Faculty of Earth and Life Sciences, VU Universiteit Amsterdam, 1081HV Amsterdam, The Netherlands. ; 1] Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus, Southampton SO14 3ZH, UK [2] Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06511, USA. ; 1] Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA [2] Department of Earth and Environmental Sciences, University of St Andrews, St Andrews KY16 9AL, UK. ; 1] Institute of Environmental Science and Technology (ICTA), Universitat Autonoma de Barcelona, Bellaterra, Catalonia, 08193, Spain [2] Department of Geography, Universitat Autonoma de Barcelona, Bellaterra, Catalonia, 08193, Spain. ; Institute of Geochemistry and Petrology, Department of Earth Sciences, ETH Zurich, NW D81.4, Zurich 8092, Switzerland.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25673416" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/chemistry ; Boron/*analysis/*chemistry ; Carbon Dioxide/*analysis ; Climate ; Foraminifera ; Freezing ; History, Ancient ; Hydrogen-Ion Concentration ; Ice Cover/*chemistry ; Isotopes ; Oceans and Seas ; Seawater/*chemistry
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  • 16
    Publication Date: 2015-11-06
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Monastersky, Richard -- England -- Nature. 2015 Nov 5;527(7576):26-9. doi: 10.1038/527026a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26536941" target="_blank"〉PubMed〈/a〉
    Keywords: Agriculture/history ; Archaeology ; Civilization/*history ; Climate ; Colorado ; Computer Simulation ; Droughts/history ; History, Medieval ; Human Migration/*history ; New Mexico ; Politics ; Time Factors ; Violence
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  • 17
    Publication Date: 2015-11-06
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Whiteman, Gail -- Hoster, Harry -- England -- Nature. 2015 Nov 5;527(7576):38. doi: 10.1038/527038a.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Lancaster University, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26536947" target="_blank"〉PubMed〈/a〉
    Keywords: Biodiversity ; Climate ; Congresses as Topic ; Conservation of Natural Resources/economics/*legislation & jurisprudence ; Environmental Policy/*legislation & jurisprudence ; Health ; Humans ; Paris ; Urban Renewal/trends ; Vehicle Emissions/*analysis/legislation & jurisprudence/*prevention & control
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    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 18
    Publication Date: 2015-03-13
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉LaDue, Nicole D -- England -- Nature. 2015 Mar 12;519(7542):131. doi: 10.1038/519131a.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Geology and Environmental Geosciences at Northern Illinois University in DeKalb.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25762247" target="_blank"〉PubMed〈/a〉
    Keywords: Climate ; Earth Sciences/*education ; Schools ; Teaching/*trends ; United States ; Weather
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    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 19
    Publication Date: 2016-04-07
    Description: As the last habitable continent colonized by humans, the site of multiple domestication hotspots, and the location of the largest Pleistocene megafaunal extinction, South America is central to human prehistory. Yet remarkably little is known about human population dynamics during colonization, subsequent expansions, and domestication. Here we reconstruct the spatiotemporal patterns of human population growth in South America using a newly aggregated database of 1,147 archaeological sites and 5,464 calibrated radiocarbon dates spanning fourteen thousand to two thousand years ago (ka). We demonstrate that, rather than a steady exponential expansion, the demographic history of South Americans is characterized by two distinct phases. First, humans spread rapidly throughout the continent, but remained at low population sizes for 8,000 years, including a 4,000-year period of 'boom-and-bust' oscillations with no net growth. Supplementation of hunting with domesticated crops and animals had a minimal impact on population carrying capacity. Only with widespread sedentism, beginning ~5 ka, did a second demographic phase begin, with evidence for exponential population growth in cultural hotspots, characteristic of the Neolithic transition worldwide. The unique extent of humanity's ability to modify its environment to markedly increase carrying capacity in South America is therefore an unexpectedly recent phenomenon.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Goldberg, Amy -- Mychajliw, Alexis M -- Hadly, Elizabeth A -- England -- Nature. 2016 Apr 14;532(7598):232-5. doi: 10.1038/nature17176. Epub 2016 Apr 6.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Biology Department, Stanford University, Stanford, California 94305, USA. ; Woods Institute, Stanford University, Stanford, California 94305, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/27049941" target="_blank"〉PubMed〈/a〉
    Keywords: Agriculture/history ; Archaeology ; Climate ; Geographic Mapping ; History, Ancient ; Human Migration/*history ; Humans ; Population Dynamics/*history ; Radiometric Dating ; Siberia/ethnology ; South America
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    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 20
    Publication Date: 2016-03-25
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Tollefson, Jeff -- England -- Nature. 2016 Mar 24;531(7595):421-2. doi: 10.1038/531421a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/27008945" target="_blank"〉PubMed〈/a〉
    Keywords: Antarctic Regions ; Climate ; Ecosystem ; Oceanography/*instrumentation/*methods ; Oceans and Seas ; Robotics/*instrumentation ; Salinity ; Seawater/chemistry ; Temperature
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  • 21
    Publication Date: 2016-02-04
    Description: No single mechanism can account for the full amplitude of past atmospheric carbon dioxide (CO2) concentration variability over glacial-interglacial cycles. A build-up of carbon in the deep ocean has been shown to have occurred during the Last Glacial Maximum. However, the mechanisms responsible for the release of the deeply sequestered carbon to the atmosphere at deglaciation, and the relative importance of deep ocean sequestration in regulating millennial-timescale variations in atmospheric CO2 concentration before the Last Glacial Maximum, have remained unclear. Here we present sedimentary redox-sensitive trace-metal records from the Antarctic Zone of the Southern Ocean that provide a reconstruction of transient changes in deep ocean oxygenation and, by inference, respired carbon storage throughout the last glacial cycle. Our data suggest that respired carbon was removed from the abyssal Southern Ocean during the Northern Hemisphere cold phases of the deglaciation, when atmospheric CO2 concentration increased rapidly, reflecting--at least in part--a combination of dwindling iron fertilization by dust and enhanced deep ocean ventilation. Furthermore, our records show that the observed covariation between atmospheric CO2 concentration and abyssal Southern Ocean oxygenation was maintained throughout most of the past 80,000 years. This suggests that on millennial timescales deep ocean circulation and iron fertilization in the Southern Ocean played a consistent role in modifying atmospheric CO2 concentration.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Jaccard, Samuel L -- Galbraith, Eric D -- Martinez-Garcia, Alfredo -- Anderson, Robert F -- England -- Nature. 2016 Feb 11;530(7589):207-10. doi: 10.1038/nature16514. Epub 2016 Feb 3.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Institute of Geological Sciences, University of Bern, Bern, Switzerland. ; Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland. ; Department of Earth and Planetary Sciences, McGill University, Montreal, Canada. ; Institucio Catalana de Recerca i Estudis Avancats (ICREA), Barcelona, Spain. ; Institut de Ciencia i Tecnologia Ambientals and Department of Mathematics, Universitat Autonoma de Barcelona, Barcelona, Spain. ; Geological Institute, ETH Zurich, Zurich, Switzerland. ; Climate Geochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany. ; Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26840491" target="_blank"〉PubMed〈/a〉
    Keywords: Antarctic Regions ; Atmosphere/*chemistry ; Carbon Dioxide/*analysis/history/metabolism ; Carbon Sequestration ; Cell Respiration ; Climate ; Dust ; Geologic Sediments/chemistry ; History, Ancient ; *Ice Cover ; Iron/analysis/chemistry ; Oceans and Seas ; Oxidation-Reduction ; Oxygen/*analysis/metabolism ; Seawater/*chemistry ; Temperature ; Water Movements
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  • 22
    Publication Date: 2016-01-15
    Description: The past rapid growth of Northern Hemisphere continental ice sheets, which terminated warm and stable climate periods, is generally attributed to reduced summer insolation in boreal latitudes. Yet such summer insolation is near to its minimum at present, and there are no signs of a new ice age. This challenges our understanding of the mechanisms driving glacial cycles and our ability to predict the next glacial inception. Here we propose a critical functional relationship between boreal summer insolation and global carbon dioxide (CO2) concentration, which explains the beginning of the past eight glacial cycles and might anticipate future periods of glacial inception. Using an ensemble of simulations generated by an Earth system model of intermediate complexity constrained by palaeoclimatic data, we suggest that glacial inception was narrowly missed before the beginning of the Industrial Revolution. The missed inception can be accounted for by the combined effect of relatively high late-Holocene CO2 concentrations and the low orbital eccentricity of the Earth. Additionally, our analysis suggests that even in the absence of human perturbations no substantial build-up of ice sheets would occur within the next several thousand years and that the current interglacial would probably last for another 50,000 years. However, moderate anthropogenic cumulative CO2 emissions of 1,000 to 1,500 gigatonnes of carbon will postpone the next glacial inception by at least 100,000 years. Our simulations demonstrate that under natural conditions alone the Earth system would be expected to remain in the present delicately balanced interglacial climate state, steering clear of both large-scale glaciation of the Northern Hemisphere and its complete deglaciation, for an unusually long time.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Ganopolski, A -- Winkelmann, R -- Schellnhuber, H J -- England -- Nature. 2016 Jan 14;529(7585):200-3. doi: 10.1038/nature16494.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Potsdam Institute for Climate Impact Research, 14412 Potsdam, Germany. ; Physics Institute, Potsdam University, 14476 Potsdam, Germany. ; Santa Fe Institute, Santa Fe, New Mexico 87501, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26762457" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/chemistry ; Carbon Dioxide/*analysis ; Climate ; Earth (Planet) ; *Ice Cover ; *Models, Theoretical ; Seasons ; Time Factors
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  • 23
    Publication Date: 2015-03-06
    Description: Over 20% of Earth's terrestrial surface is underlain by permafrost with vast stores of carbon that, once thawed, may represent the largest future transfer of carbon from the biosphere to the atmosphere. This process is largely dependent on microbial responses, but we know little about microbial activity in intact, let alone in thawing, permafrost. Molecular approaches have recently revealed the identities and functional gene composition of microorganisms in some permafrost soils and a rapid shift in functional gene composition during short-term thaw experiments. However, the fate of permafrost carbon depends on climatic, hydrological and microbial responses to thaw at decadal scales. Here we use the combination of several molecular 'omics' approaches to determine the phylogenetic composition of the microbial communities, including several draft genomes of novel species, their functional potential and activity in soils representing different states of thaw: intact permafrost, seasonally thawed active layer and thermokarst bog. The multi-omics strategy reveals a good correlation of process rates to omics data for dominant processes, such as methanogenesis in the bog, as well as novel survival strategies for potentially active microbes in permafrost.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Hultman, Jenni -- Waldrop, Mark P -- Mackelprang, Rachel -- David, Maude M -- McFarland, Jack -- Blazewicz, Steven J -- Harden, Jennifer -- Turetsky, Merritt R -- McGuire, A David -- Shah, Manesh B -- VerBerkmoes, Nathan C -- Lee, Lang Ho -- Mavrommatis, Kostas -- Jansson, Janet K -- England -- Nature. 2015 May 14;521(7551):208-12. doi: 10.1038/nature14238. Epub 2015 Mar 4.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Earth Sciences Division, Lawrence Berkeley National Laboratory, 1 Cyclotron Road, Berkeley, California, 94720, USA. ; US Geological Survey, 345 Middlefield Road, Menlo Park, California 94025, USA. ; 1] Biology Department, 18111 Nordhoff Street, California State University Northridge, Northridge, California 91330, USA [2] US Department of Energy Joint Genome Institute, 2800 Mitchell Drive, Walnut Creek, California 94598, USA. ; Department of Integrative Biology, 50 Stone Road East, University of Guelph, Guelph, Ontario N1G 2W1, Canada. ; US Geological Survey, Alaska Cooperative Fish and Wildlife Research Unit, 211A Irving I Building, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USA. ; Chemical Sciences Division, One Bethel Valley Road, Building 1059, Oak Ridge National Laboratory, Oak Ridge, Tennessee 37831-6420, USA. ; Graduate School of Genome Science and Technology, University of Tennessee and Oak Ridge National Laboratory, 2510 River Drive, Knoxville, Tennessee 37996, USA. ; US Department of Energy Joint Genome Institute, 2800 Mitchell Drive, Walnut Creek, California 94598, USA. ; 1] Earth Sciences Division, Lawrence Berkeley National Laboratory, 1 Cyclotron Road, Berkeley, California, 94720, USA [2] US Department of Energy Joint Genome Institute, 2800 Mitchell Drive, Walnut Creek, California 94598, USA [3] Department of Plant and Microbial Biology, 111 Koshland Hall, University of California, Berkeley, Berkeley, California 94720, USA [4] Center for Permafrost Research (CENPERM), Department of Biology, Universitetsparken 15, University of Copenhagen, Copenhagen, DK-2100 Copenhagen, Denmark.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25739499" target="_blank"〉PubMed〈/a〉
    Keywords: Alaska ; Atmosphere/chemistry ; Carbon Cycle ; Climate ; Denitrification ; Freezing ; Genome, Bacterial/*genetics ; Iron/metabolism ; Metagenome/*genetics ; Methane/metabolism ; Microbiota/genetics/*physiology ; Nitrates/metabolism ; Nitrogen/metabolism ; Oxidation-Reduction ; Permafrost/*microbiology ; Phylogeny ; Seasons ; *Soil Microbiology ; Sulfur/metabolism ; Time Factors ; *Wetlands
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    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 24
    Publication Date: 2022-05-25
    Description: Author Posting. © Annual Reviews, 2003. This article is posted here by permission of Annual Reviews for personal use, not for redistribution. The definitive version was published in Annual Review of Environment and Resources 28 (2003): 521-558, doi:10.1146/annurev.energy.28.011503.163443.
    Description: Agriculture and industrial development have led to inadvertent changes in the natural carbon cycle. As a consequence, concentrations of carbon dioxide and other greenhouse gases have increased in the atmosphere and may lead to changes in climate. The current challenge facing society is to develop options for future management of the carbon cycle. A variety of approaches has been suggested: direct reduction of emissions, deliberate manipulation of the natural carbon cycle to enhance sequestration, and capture and isolation of carbon from fossil fuel use. Policy development to date has laid out some of the general principles to which carbon management should adhere. These are summarized as: how much carbon is stored, by what means, and for how long. To successfully manage carbon for climate purposes requires increased understanding of carbon cycle dynamics and improvement in the scientific capabilities available for measurement as well as for policy needs. The specific needs for scientific information to underpin carbon cycle management decisions are not yet broadly known. A stronger dialogue between decision makers and scientists must be developed to foster improved application of scientific knowledge to decisions. This review focuses on the current knowledge of the carbon cycle, carbon measurement capabilities (with an emphasis on the continental scale) and the relevance of carbon cycle science to carbon sequestration goals.
    Description: The National Center for Atmospheric Research is supported by the National Science Foundation.
    Keywords: Carbon sequestration ; Measurement techniques ; Climate ; Kyoto protocol
    Repository Name: Woods Hole Open Access Server
    Type: Article
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