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  • 1
    Publication Date: 2006
    Keywords: Source parameters ; Earthquake ; historical ; Seismicity ; Structural geology ; JGR ; Sumatra ; paleoseismology ; 7221 ; Seismology: ; Paleoseismology ; 9340 ; Geographic ; Location: ; Indian ; Ocean ; 7240 ; Seismology: ; Subduction ; zones ; 1120 ; Geochronology: ; Isotopic ; disequilibrium ; dating
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  • 2
    Publication Date: 2011-04-01
    Description: Pleistocene water intrusions from the Mediterranean and Caspian seas into the Black Sea Nature Geoscience 4, 236 (2011). doi:10.1038/ngeo1106 Authors: S. Badertscher, D. Fleitmann, H. Cheng, R. L. Edwards, O. M. Göktürk, A. Zumbühl, M. Leuenberger & O. Tüysüz The hydrological balance of the Black Sea is governed by riverine input and by the exchange with the Mediterranean Sea through the shallow Bosporus Strait. These sources have distinctly different oxygen isotope (δ18O) signatures. Therefore, the δ18O of Black Sea water directly reflects the presence or absence of a connection with the Mediterranean Sea, as well as hydrological changes in the vast watersheds of the Black and Caspian seas. However, the timing of late to middle Pleistocene water intrusions to the Black Sea is poorly constrained in sedimentary sequences. Here we present a stacked speleothem δ18O record from Sofular Cave in northern Turkey that tracks the isotopic signature of Black Sea surface water, and thus allows a reconstruction of the precise timing of hydrological shifts of the Black Sea. Our record, which extends discontinuously over the last 670,000 years, suggests that the connection between the Black Sea and Mediterranean Sea has been open for a significant period at least twelve times since 670,000 yr ago, more often than previously suggested. Distinct minima in the Sofular δ18O record indicate at least seven intervals when isotopically depleted freshwater from the Caspian Sea entered the Black Sea. Our data provide precisely dated evidence for a highly dynamic hydrological history of the Black Sea.
    Print ISSN: 1752-0894
    Electronic ISSN: 1752-0908
    Topics: Geosciences
    Published by Springer Nature
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  • 3
    Publication Date: 2015-10-09
    Description: The Levant constitutes an important region for assessing linkages between climate and societal changes throughout the course of human history. However, large uncertainties remain in our understanding of the region's hydroclimate variability under varying boundary conditions. Here we present a new high-resolution, precisely-dated speleothem oxygen-carbon isotope and Sr/Ca records, spanning the last 20ka from Jeita Cave, northern Levant. Our record reveals a higher (lower) precipitation-evaporation (P-E) balance during the Last Glacial Maximum and Bølling interstadial (Heinrich stadial 1). The early-mid Holocene is characterized by a trend towards higher P-E state, culminating between ~7 and 6 ka BP. The mid-late Holocene is characterized by two millennial-length drier periods during 5.3–4.2 and 2.8–1.4ka BP. On sub-millennial scale, the northern Levant climate variability is dominated by 500-year periodicity. Comparisons with the regional proxy records suggest persistent out-of-phase climate variability between the northern and southern Levant on a wide-range of timescales.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 4
    Publication Date: 2012-01-13
    Description: Central Asia is currently a semiarid-arid region, dominated by the Westerlies. It is important to understand mechanisms of climate and precipitation changes here, as water availability in the region is crucial today and in the future. High-resolution, absolutely-dated oxygen isotope (δ18O) records of stalagmites from Kesang Cave characterize a dynamic precipitation history over most of the past 500,000 years. This record demonstrates, for the first time, that climate change in the region exhibits a processional rhythm with abrupt inceptions of low δ18O speleothem growth at times of high Northern Hemisphere summer insolation followed by gradual δ18O increases that track decreases of insolation. These observations and interpretations contrast with the interpretation of nearby, but higher elevation ice core records. The absolutely-dated cave δ18O shifts can be used to correlate the regional climate variability by providing chronological marks. Combined with other paleoclimate records, the Kesang observations suggest that possible incursions of Asian summer monsoon rainfall or related moisture into the Kesang site and/or adjacent areas during the high insolation times may play an important role in changing orbital-scale hydrology of the region. Based on our record, arid climate will prevail in this region for the next several millennia, providing that anthropogenic effects do not supersede natural processes.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 5
    Publication Date: 2014-09-27
    Description: Article Detailed sea-level records beyond ~150,000 years ago are limited. Here, the authors present a radiometrically constrained sea-level record from the Red Sea, spanning five glacial cycles and examine sea-level rise rates and the effects of past global ice-volume changes on monsoon intensity. Nature Communications doi: 10.1038/ncomms6076 Authors: K. M. Grant, E. J. Rohling, C. Bronk Ramsey, H. Cheng, R. L. Edwards, F. Florindo, D. Heslop, F. Marra, A. P. Roberts, M. E. Tamisiea, F. Williams
    Electronic ISSN: 2041-1723
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General , Physics
    Published by Springer Nature
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  • 6
    Publication Date: 2001-12-18
    Description: Oxygen isotope records of five stalagmites from Hulu Cave near Nanjing bear a remarkable resemblance to oxygen isotope records from Greenland ice cores, suggesting that East Asian Monsoon intensity changed in concert with Greenland temperature between 11,000 and 75,000 years before the present (yr. B.P.). Between 11,000 and 30,000 yr. B.P., the timing of changes in the monsoon, as established with 230Th dates, generally agrees with the timing of temperature changes from the Greenland Ice Sheet Project Two (GISP2) core, which supports GISP2's chronology in this interval. Our record links North Atlantic climate with the meridional transport of heat and moisture from the warmest part of the ocean where the summer East Asian Monsoon originates.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Wang, Y J -- Cheng, H -- Edwards, R L -- An, Z S -- Wu, J Y -- Shen, C C -- Dorale, J A -- New York, N.Y. -- Science. 2001 Dec 14;294(5550):2345-8.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉College of Geography Science, Nanjing Normal University, Nanjing 210097, China.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/11743199" 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: 2001-05-12
    Description: A long record of atmospheric 14C concentration, from 45 to 11 thousand years ago (ka), was obtained from a stalagmite with thermal-ionization mass-spectrometric 230Th and accelerator mass-spectrometric 14C measurements. This record reveals highly elevated Delta14C between 45 and 33 ka, portions of which may correlate with peaks in cosmogenic 36Cl and 10Be isotopes observed in polar ice cores. Superimposed on this broad peak of Delta14C are several rapid excursions, the largest of which occurs between 44.3 and 43.3 ka. Between 26 and 11 ka, atmospheric Delta14C decreased from approximately 700 to approximately 100 per mil, modulated by numerous minor excursions. Carbon cycle models suggest that the major features of this record cannot be produced with solar or terrestrial magnetic field modulation alone but also require substantial fluctuations in the carbon cycle.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Beck, J W -- Richards, D A -- Edwards, R L -- Silverman, B W -- Smart, P L -- Donahue, D J -- Hererra-Osterheld, S -- Burr, G S -- Calsoyas, L -- Jull, A J -- Biddulph, D -- New York, N.Y. -- Science. 2001 Jun 29;292(5526):2453-8. Epub 2001 May 10.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉NSF-Arizona Accelerator Mass Spectrometry Facility, Department of Physics, University of Arizona, Tucson, AZ 85721, USA. wbeck@physics.arizona.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/11349137" 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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  • 8
    Publication Date: 1998-05-13
    Description: Coupled radiocarbon and thorium-230 dates from benthic coral species reveal that the ventilation rate of the North Atlantic upper deep water varied greatly during the last deglaciation. Radiocarbon ages in several corals of the same age, 15.41 +/- 0.17 thousand years, and nearly the same depth, 1800 meters, in the western North Atlantic Ocean increased by as much as 670 years during the 30- to 160-year life spans of the samples. Cadmium/calcium ratios in one coral imply that the nutrient content of these deep waters also increased. Our data show that the deep ocean changed on decadal-centennial time scales during rapid changes in the surface ocean and the atmosphere.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Adkins -- Cheng -- Boyle -- Druffel -- Edwards -- New York, N.Y. -- Science. 1998 May 1;280(5364):725-8.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉J. F. Adkins and E. A. Boyle, Department of Earth, Atmosphere and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA. H. Cheng and R. L. Edwards, Department of Geology and Geophysics, University of Minnesota, Minne.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/9563946" 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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  • 9
    Publication Date: 1998-12-04
    Description: Four Missouri stalagmites yield consistent overlapping records of oxygen and carbon isotopic changes and provide a climate and vegetation history with submillennial resolution from 75 to 25 thousand years ago (ka). The thorium-230-dated records reveal that between 75 and 55 ka, the midcontinental climate oscillated on millennial time scales between cold and warm, and vegetation alternated among forest, savanna, and prairie. Temperatures were highest and prairie vegetation peaked between 59 and 55 ka. Climate cooled and forest replaced grassland at 55 ka, when global ice sheets began to build during the early part of Marine Oxygen Isotope Stage 3.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Dorale -- Edwards -- Ito -- Gonzalez -- New York, N.Y. -- Science. 1998 Dec 4;282(5395):1871-4.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉J. A. Dorale, R. L. Edwards, E. Ito, Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA. L. A. Gonzalez, Department of Geology, University of Iowa, Iowa City, IA 52242, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/9836633" 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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  • 10
    Publication Date: 2008-02-29
    Description: High-resolution speleothem records from China have provided insights into the factors that control the strength of the East Asian monsoon. Our understanding of these factors remains incomplete, however, owing to gaps in the record of monsoon history over the past two interglacial-glacial cycles. In particular, missing sections have hampered our ability to test ideas about orbital-scale controls on the monsoon, the causes of millennial-scale events and relationships between changes in the monsoon and climate in other regions. Here we present an absolute-dated oxygen isotope record from Sanbao cave, central China, that completes a Chinese-cave-based record of the strength of the East Asian monsoon that covers the past 224,000 years. The record is dominated by 23,000-year-long cycles that are synchronous within dating errors with summer insolation at 65 degrees N (ref. 10), supporting the idea that tropical/subtropical monsoons respond dominantly and directly to changes in Northern Hemisphere summer insolation on orbital timescales. The cycles are punctuated by millennial-scale strong-summer-monsoon events (Chinese interstadials), and the new record allows us to identify the complete series of these events over the past two interglacial-glacial cycles. Their duration decreases and their frequency increases during glacial build-up in both the last and penultimate glacial periods, indicating that ice sheet size affects their character and pacing. The ages of the events are exceptionally well constrained and may thus serve as benchmarks for correlating and calibrating climate records.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Wang, Yongjin -- Cheng, Hai -- Edwards, R Lawrence -- Kong, Xinggong -- Shao, Xiaohua -- Chen, Shitao -- Wu, Jiangyin -- Jiang, Xiouyang -- Wang, Xianfeng -- An, Zhisheng -- England -- Nature. 2008 Feb 28;451(7182):1090-3. doi: 10.1038/nature06692.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉College of Geography Science, Nanjing Normal University, Nanjing, Jiangsu 210097, China. yjwang@njnu.edu.cn〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18305541" 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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