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  • 1
    Publication Date: 2013-10-18
    Description: ABSTRACT Nineteen new Icelandic tephra layers are identified in NGRIP and NEEM ice spanning Greenland Interstadial-9 (GI-9) and the early phase of GI-8 (∼38 000–40 500 b2k). Fourteen tephras are identified in the NGRIP record and five direct correlatives are identified in NEEM, thus indicating the occurrence of 14 separate volcanic events. With two exceptions, the tephras are tholeiitic basalt in composition and despite having very similar geochemical signatures can, in most cases, be discriminated from one another using their TiO 2 values. All of these tephra layers fall within the compositional range of the Faroe Marine Ash Zone III (FMAZ III) deposit previously identified in ocean cores from the Faroes region and previously correlated to NGRIP 2066.95 m by Davies et al . ( ). Thus, the FMAZ III in the marine realm is most likely a complex ash zone that represents a series of closely timed Grimsvötn eruptions that, as yet, can only be stratigraphically separated in the high-resolution ice-core records. The geochemical signatures and stratigraphic positions of the new ice-core layers means that the FMAZ III tephra deposit, as currently defined in the marine realm, cannot be correlated to NGRIP 2066.95 m or any other ice-core tephra horizons preserved during this interval.
    Print ISSN: 0267-8179
    Electronic ISSN: 1099-1417
    Topics: Geography , Geosciences
    Published by Wiley
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  • 2
    Publication Date: 2008-04-04
    Description: Dust can affect the radiative balance of the atmosphere by absorbing or reflecting incoming solar radiation; it can also be a source of micronutrients, such as iron, to the ocean. It has been suggested that production, transport and deposition of dust is influenced by climatic changes on glacial-interglacial timescales. Here we present a high-resolution record of aeolian dust from the EPICA Dome C ice core in East Antarctica, which provides an undisturbed climate sequence over the past eight climatic cycles. We find that there is a significant correlation between dust flux and temperature records during glacial periods that is absent during interglacial periods. Our data suggest that dust flux is increasingly correlated with Antarctic temperature as the climate becomes colder. We interpret this as progressive coupling of the climates of Antarctic and lower latitudes. Limited changes in glacial-interglacial atmospheric transport time suggest that the sources and lifetime of dust are the main factors controlling the high glacial dust input. We propose that the observed approximately 25-fold increase in glacial dust flux over all eight glacial periods can be attributed to a strengthening of South American dust sources, together with a longer lifetime for atmospheric dust particles in the upper troposphere resulting from a reduced hydrological cycle during the ice ages.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Lambert, F -- Delmonte, B -- Petit, J R -- Bigler, M -- Kaufmann, P R -- Hutterli, M A -- Stocker, T F -- Ruth, U -- Steffensen, J P -- Maggi, V -- England -- Nature. 2008 Apr 3;452(7187):616-9. doi: 10.1038/nature06763.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18385736" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2009-09-18
    Description: On entering an era of global warming, the stability of the Greenland ice sheet (GIS) is an important concern, especially in the light of new evidence of rapidly changing flow and melt conditions at the GIS margins. Studying the response of the GIS to past climatic change may help to advance our understanding of GIS dynamics. The previous interpretation of evidence from stable isotopes (delta(18)O) in water from GIS ice cores was that Holocene climate variability on the GIS differed spatially and that a consistent Holocene climate optimum-the unusually warm period from about 9,000 to 6,000 years ago found in many northern-latitude palaeoclimate records-did not exist. Here we extract both the Greenland Holocene temperature history and the evolution of GIS surface elevation at four GIS locations. We achieve this by comparing delta(18)O from GIS ice cores with delta(18)O from ice cores from small marginal icecaps. Contrary to the earlier interpretation of delta(18)O evidence from ice cores, our new temperature history reveals a pronounced Holocene climatic optimum in Greenland coinciding with maximum thinning near the GIS margins. Our delta(18)O-based results are corroborated by the air content of ice cores, a proxy for surface elevation. State-of-the-art ice sheet models are generally found to be underestimating the extent and changes in GIS elevation and area; our findings may help to improve the ability of models to reproduce the GIS response to Holocene climate.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Vinther, B M -- Buchardt, S L -- Clausen, H B -- Dahl-Jensen, D -- Johnsen, S J -- Fisher, D A -- Koerner, R M -- Raynaud, D -- Lipenkov, V -- Andersen, K K -- Blunier, T -- Rasmussen, S O -- Steffensen, J P -- Svensson, A M -- England -- Nature. 2009 Sep 17;461(7262):385-8. doi: 10.1038/nature08355.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Juliane Maries Vej 30, DK-2100 Copenhagen Oe, Denmark. bo@gfy.ku.dk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19759618" target="_blank"〉PubMed〈/a〉
    Keywords: Altitude ; *Greenhouse Effect ; Greenland ; History, Ancient ; *Ice Cover ; Oxygen/analysis ; Oxygen Isotopes ; Temperature
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2007-07-07
    Description: It is difficult to obtain fossil data from the 10% of Earth's terrestrial surface that is covered by thick glaciers and ice sheets, and hence, knowledge of the paleoenvironments of these regions has remained limited. We show that DNA and amino acids from buried organisms can be recovered from the basal sections of deep ice cores, enabling reconstructions of past flora and fauna. We show that high-altitude southern Greenland, currently lying below more than 2 kilometers of ice, was inhabited by a diverse array of conifer trees and insects within the past million years. The results provide direct evidence in support of a forested southern Greenland and suggest that many deep ice cores may contain genetic records of paleoenvironments in their basal sections.〈br /〉〈br /〉〈a href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC2694912/" 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/PMC2694912/" target="_blank"〉This paper as free author manuscript - peer-reviewed and accepted for publication〈/a〉〈br /〉〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Willerslev, Eske -- Cappellini, Enrico -- Boomsma, Wouter -- Nielsen, Rasmus -- Hebsgaard, Martin B -- Brand, Tina B -- Hofreiter, Michael -- Bunce, Michael -- Poinar, Hendrik N -- Dahl-Jensen, Dorthe -- Johnsen, Sigfus -- Steffensen, Jorgen Peder -- Bennike, Ole -- Schwenninger, Jean-Luc -- Nathan, Roger -- Armitage, Simon -- de Hoog, Cees-Jan -- Alfimov, Vasily -- Christl, Marcus -- Beer, Juerg -- Muscheler, Raimund -- Barker, Joel -- Sharp, Martin -- Penkman, Kirsty E H -- Haile, James -- Taberlet, Pierre -- Gilbert, M Thomas P -- Casoli, Antonella -- Campani, Elisa -- Collins, Matthew J -- 076905/Wellcome Trust/United Kingdom -- Wellcome Trust/United Kingdom -- New York, N.Y. -- Science. 2007 Jul 6;317(5834):111-4.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Centre for Ancient Genetics, University of Copenhagen, Denmark. ewillerslev@bi.ku.dk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17615355" target="_blank"〉PubMed〈/a〉
    Keywords: Amino Acids/*analysis/history/isolation & purification ; Animals ; Bayes Theorem ; Climate ; DNA/*analysis/history/isolation & purification ; *Ecosystem ; Fossils ; Geography ; Greenland ; History, Ancient ; Ice Cover/*chemistry ; *Invertebrates/classification/genetics ; *Plants/classification/genetics ; Polymerase Chain Reaction ; Time ; *Trees
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 5
    Publication Date: 2007-07-07
    Description: A high-resolution deuterium profile is now available along the entire European Project for Ice Coring in Antarctica Dome C ice core, extending this climate record back to marine isotope stage 20.2, approximately 800,000 years ago. Experiments performed with an atmospheric general circulation model including water isotopes support its temperature interpretation. We assessed the general correspondence between Dansgaard-Oeschger events and their smoothed Antarctic counterparts for this Dome C record, which reveals the presence of such features with similar amplitudes during previous glacial periods. We suggest that the interplay between obliquity and precession accounts for the variable intensity of interglacial periods in ice core records.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Jouzel, J -- Masson-Delmotte, V -- Cattani, O -- Dreyfus, G -- Falourd, S -- Hoffmann, G -- Minster, B -- Nouet, J -- Barnola, J M -- Chappellaz, J -- Fischer, H -- Gallet, J C -- Johnsen, S -- Leuenberger, M -- Loulergue, L -- Luethi, D -- Oerter, H -- Parrenin, F -- Raisbeck, G -- Raynaud, D -- Schilt, A -- Schwander, J -- Selmo, E -- Souchez, R -- Spahni, R -- Stauffer, B -- Steffensen, J P -- Stenni, B -- Stocker, T F -- Tison, J L -- Werner, M -- Wolff, E W -- New York, N.Y. -- Science. 2007 Aug 10;317(5839):793-6. Epub 2007 Jul 5.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Laboratoire des Sciences du Climat et l'Environnement, Institut Pierre Simon Laplace, CEA-CNRS-Universite de Versailles Saint-Quentin en Yvelines, CE Saclay, Gif-sur-Yvette, France. jean.jouzel@lsce.ipsl.fr〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17615306" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 6
    Publication Date: 2008-06-21
    Description: The last two abrupt warmings at the onset of our present warm interglacial period, interrupted by the Younger Dryas cooling event, were investigated at high temporal resolution from the North Greenland Ice Core Project ice core. The deuterium excess, a proxy of Greenland precipitation moisture source, switched mode within 1 to 3 years over these transitions and initiated a more gradual change (over 50 years) of the Greenland air temperature, as recorded by stable water isotopes. The onsets of both abrupt Greenland warmings were slightly preceded by decreasing Greenland dust deposition, reflecting the wetting of Asian deserts. A northern shift of the Intertropical Convergence Zone could be the trigger of these abrupt shifts of Northern Hemisphere atmospheric circulation, resulting in changes of 2 to 4 kelvin in Greenland moisture source temperature from one year to the next.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Steffensen, Jorgen Peder -- Andersen, Katrine K -- Bigler, Matthias -- Clausen, Henrik B -- Dahl-Jensen, Dorthe -- Fischer, Hubertus -- Goto-Azuma, Kumiko -- Hansson, Margareta -- Johnsen, Sigfus J -- Jouzel, Jean -- Masson-Delmotte, Valerie -- Popp, Trevor -- Rasmussen, Sune O -- Rothlisberger, Regine -- Ruth, Urs -- Stauffer, Bernhard -- Siggaard-Andersen, Marie-Louise -- Sveinbjornsdottir, Arny E -- Svensson, Anders -- White, James W C -- New York, N.Y. -- Science. 2008 Aug 1;321(5889):680-4. doi: 10.1126/science.1157707. Epub 2008 Jun 19.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Juliane Maries Vej 30, DK-2100 Copenhagen OE, Denmark. jps@gfy.ku.dk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18566247" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 7
    Publication Date: 2012-11-15
    Description: Acidity peaks in Greenland ice cores have been used as critical reference horizons for synchronizing ice core records, aiding the construction of a single Greenland Ice Core Chronology (GICC05) for the Holocene. Guided by GICC05, we examined sub-sections of three Greenland cores in the search for tephra from specific eruptions that might facilitate the linkage of ice core records, the dating of prehistoric tephras and the understanding of the eruptions. Here we report the identification of 14 horizons with tephra particles, including 11 that have not previously been reported from the North Atlantic region and that have the potential to be valuable isochrons. The positions of tephras whose major element data are consistent with ash from the Katmai AD 1912 and Öraefajökull AD 1362 eruptions confirm the annually resolved ice core chronology for the last 700 years. We provide a more refined date for the so-called “AD860B” tephra, a widespread isochron found across NW Europe, and present new evidence relating to the 17th century BC Thera/Aniakchak debate that shows N. American eruptions likely contributed to the acid signals at this time. Our results emphasize the variable spatial and temporal distributions of volcanic products in Greenland ice that call for a more cautious approach in the attribution of acid signals to specific eruptive events.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 8
    Publication Date: 2015-07-15
    Description: Volcanic eruptions contribute to climate variability, but quantifying these contributions has been limited by inconsistencies in the timing of atmospheric volcanic aerosol loading determined from ice cores and subsequent cooling from climate proxies such as tree rings. Here we resolve these inconsistencies and show that large eruptions in the tropics and high latitudes were primary drivers of interannual-to-decadal temperature variability in the Northern Hemisphere during the past 2,500 years. Our results are based on new records of atmospheric aerosol loading developed from high-resolution, multi-parameter measurements from an array of Greenland and Antarctic ice cores as well as distinctive age markers to constrain chronologies. Overall, cooling was proportional to the magnitude of volcanic forcing and persisted for up to ten years after some of the largest eruptive episodes. Our revised timescale more firmly implicates volcanic eruptions as catalysts in the major sixth-century pandemics, famines, and socioeconomic disruptions in Eurasia and Mesoamerica while allowing multi-millennium quantification of climate response to volcanic forcing.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Sigl, M -- Winstrup, M -- McConnell, J R -- Welten, K C -- Plunkett, G -- Ludlow, F -- Buntgen, U -- Caffee, M -- Chellman, N -- Dahl-Jensen, D -- Fischer, H -- Kipfstuhl, S -- Kostick, C -- Maselli, O J -- Mekhaldi, F -- Mulvaney, R -- Muscheler, R -- Pasteris, D R -- Pilcher, J R -- Salzer, M -- Schupbach, S -- Steffensen, J P -- Vinther, B M -- Woodruff, T E -- England -- Nature. 2015 Jul 30;523(7562):543-9. doi: 10.1038/nature14565. Epub 2015 Jul 8.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Desert Research Institute, Nevada System of Higher Education, Reno, Nevada 89512, USA. ; Department of Earth and Space Sciences, University of Washington, Seattle, Washington 98195, USA. ; Space Sciences Laboratory, University of California, Berkeley, California 94720, USA. ; School of Geography, Archaeology and Palaeoecology, Queen's University Belfast, Belfast BT7 1NN, UK. ; Yale Climate and Energy Institute, and Department of History, Yale University, New Haven, Connecticut 06511, USA. ; 1] Swiss Federal Research Institute WSL, 8903 Birmensdorf, Switzerland [2] Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland [3] Global Change Research Centre AS CR, 60300 Brno, Czech Republic. ; 1] Department of Physics, Purdue University, West Lafayette, Indiana 47907, USA [2] Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, Indiana 47907, USA. ; Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, 2100 Copenhagen, Denmark. ; 1] Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland [2] Climate and Environmental Physics, University of Bern, 3012 Bern, Switzerland. ; Alfred-Wegener-Institut Helmholtz-Zentrum fur Polar- und Meeresforschung, 27570 Bremerhaven, Germany. ; Department of History, The University of Nottingham, Nottingham NG7 2RD, UK. ; Department of Geology, Quaternary Sciences, Lund University, 22362 Lund, Sweden. ; British Antarctic Survey, Natural Environment Research Council, Cambridge CB3 0ET, UK. ; The Laboratory of Tree-Ring Research, University of Arizona, Tucson, Arizona 85721, USA. ; Department of Physics, Purdue University, West Lafayette, Indiana 47907, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26153860" target="_blank"〉PubMed〈/a〉
    Keywords: Aerosols/analysis ; Americas ; Antarctic Regions ; Atmosphere/chemistry ; Beryllium ; Carbon Radioisotopes ; *Climate ; Disasters/history ; Europe ; Greenland ; History, Ancient ; History, Medieval ; Ice/analysis ; Radioisotopes ; Radiometric Dating ; Seasons ; Sulfur ; *Temperature ; Time Factors ; Trees/anatomy & histology/growth & development ; Tropical Climate ; Volcanic Eruptions/*history
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 9
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] In 1990-92, the joint European Greenland Ice-core Project (GRIP) drilled an ice core to near the bedrock at the very top of the Greenland ice sheet (72.58° N, 37.64° W; 3,238 m above sea level7; annual mean air temperature -32 °C). The 3,028.8-m-long core was recovered by an ...
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  • 10
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Three deep Greenland ice cores, drilled from surface to bed-rock at Camp Century, Dye 3 and Renland (Fig. 1) in 1966, 1981 and 1987, respectively, reach the ice deposited during the last glaciation1'3. This conclusion is based on the occurrence of very low 518O values (618O is the relative ...
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