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  • 1
    Publication Date: 2001-10-06
    Description: Columnar stalagmites in caves of the Guadalupe Mountains during the late Holocene record a 4000-year annually resolved climate history for the southwestern United States. Annual banding, hiatuses, and high-precision uranium-series dating show a present day-like climate from 4000 to 3000 years ago, following a drier middle Holocene. A distinctly wetter and cooler period from 3000 to 800 years ago was followed by a period of present day-like conditions, with the exception of a slightly wetter interval from 440 to 290 years before the present. The stalagmite record correlates well with the archaeological record of changes in cultural activities of indigenous people. Such climate change may help to explain evidence of dwelling abandonment and population redistribution.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Polyak, V J -- Asmerom, Y -- New York, N.Y. -- Science. 2001 Oct 5;294(5540):148-51.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth and Planetary Sciences, University of New Mexico, 200 Yale Boulevard, Albuquerque, NM 87131, USA. polyak@unm.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/11588259" target="_blank"〉PubMed〈/a〉
    Keywords: Agriculture ; Animals ; *Archaeology ; *Climate ; *Culture ; Fossils ; *Geologic Sediments ; Humans ; Humidity ; New Mexico ; Population Dynamics ; Population Growth ; Southwestern United States
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2012-11-10
    Description: The role of climate change in the development and demise of Classic Maya civilization (300 to 1000 C.E.) remains controversial because of the absence of well-dated climate and archaeological sequences. We present a precisely dated subannual climate record for the past 2000 years from Yok Balum Cave, Belize. From comparison of this record with historical events compiled from well-dated stone monuments, we propose that anomalously high rainfall favored unprecedented population expansion and the proliferation of political centers between 440 and 660 C.E. This was followed by a drying trend between 660 and 1000 C.E. that triggered the balkanization of polities, increased warfare, and the asynchronous disintegration of polities, followed by population collapse in the context of an extended drought between 1020 and 1100 C.E.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kennett, Douglas J -- Breitenbach, Sebastian F M -- Aquino, Valorie V -- Asmerom, Yemane -- Awe, Jaime -- Baldini, James U L -- Bartlein, Patrick -- Culleton, Brendan J -- Ebert, Claire -- Jazwa, Christopher -- Macri, Martha J -- Marwan, Norbert -- Polyak, Victor -- Prufer, Keith M -- Ridley, Harriet E -- Sodemann, Harald -- Winterhalder, Bruce -- Haug, Gerald H -- New York, N.Y. -- Science. 2012 Nov 9;338(6108):788-91. doi: 10.1126/science.1226299.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Anthropology, Pennsylvania State University, University Park, PA 16802, USA. djk23@psu.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23139330" target="_blank"〉PubMed〈/a〉
    Keywords: Agriculture/history ; Belize ; Caves ; Civilization/*history ; Climate Change/*history ; Droughts/history ; History, Ancient ; Humans ; Indians, Central American/*history ; Oxygen Isotopes ; Political Systems/*history ; *Rain ; Warfare
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2014-07-26
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Kennett, Douglas J -- Asmerom, Yemane -- Kemp, Brian M -- Polyak, Victor -- Bolnick, Deborah A -- Malhi, Ripan S -- Culleton, Brendan J -- New York, N.Y. -- Science. 2014 Jul 25;345(6195):390. doi: 10.1126/science.345.6195.390-a. Epub 2014 Jul 24.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Anthropology and Institutes of Energy and the Environment, Pennsylvania State University, University Park, PA 16802, USA. djk23@psu.edu. ; Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131-0001, USA. ; Department of Anthropology and School of Biological Sciences, Washington State University, Pullman, WA 99164, USA. ; Department of Anthropology and Population Research Center, University of Texas at Austin, Austin, TX 78712, USA. ; Institute of Genomic Biology, University of Illinois, Urbana-Champaign, IL 61801, USA. ; Department of Anthropology and Institutes of Energy and the Environment, Pennsylvania State University, University Park, PA 16802, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25061196" target="_blank"〉PubMed〈/a〉
    Keywords: *Biological Evolution ; Humans ; Indians, North American/*genetics ; *Skeleton
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2008-03-08
    Description: The age and evolution of the Grand Canyon have been subjects of great interest and debate since its discovery. We found that cave mammillaries (water table indicator speleothems) from nine sites in the Grand Canyon showed uranium-lead dating evidence for an old western Grand Canyon on the assumption that groundwater table decline rates are equivalent to incision rates. Samples in the western Grand Canyon yielded apparent water table decline rates of 55 to 123 meters per million years over the past 17 million years, in contrast to eastern Grand Canyon samples that yielded much faster rates (166 to 411 meters per million years). Chronology and inferred incision data indicate that the Grand Canyon evolved via headward erosion from west to east, together with late-stage ( approximately 3.7 million years ago) accelerated incision in the eastern block.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Polyak, Victor -- Hill, Carol -- Asmerom, Yemane -- New York, N.Y. -- Science. 2008 Mar 7;319(5868):1377-80. doi: 10.1126/science.1151248.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131, USA. polyak@unm.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18323451" 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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  • 5
    Publication Date: 2013-01-05
    Description: We report data on the martian meteorite Northwest Africa (NWA) 7034, which shares some petrologic and geochemical characteristics with known martian meteorites of the SNC (i.e., shergottite, nakhlite, and chassignite) group, but also has some unique characteristics that would exclude it from that group. NWA 7034 is a geochemically enriched crustal rock compositionally similar to basalts and average martian crust measured by recent Rover and Orbiter missions. It formed 2.089 +/- 0.081 billion years ago, during the early Amazonian epoch in Mars' geologic history. NWA 7034 has an order of magnitude more indigenous water than most SNC meteorites, with up to 6000 parts per million extraterrestrial H(2)O released during stepped heating. It also has bulk oxygen isotope values of Delta(17)O = 0.58 +/- 0.05 per mil and a heat-released water oxygen isotope average value of Delta(17)O = 0.330 +/- 0.011 per mil, suggesting the existence of multiple oxygen reservoirs on Mars.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Agee, Carl B -- Wilson, Nicole V -- McCubbin, Francis M -- Ziegler, Karen -- Polyak, Victor J -- Sharp, Zachary D -- Asmerom, Yemane -- Nunn, Morgan H -- Shaheen, Robina -- Thiemens, Mark H -- Steele, Andrew -- Fogel, Marilyn L -- Bowden, Roxane -- Glamoclija, Mihaela -- Zhang, Zhisheng -- Elardo, Stephen M -- New York, N.Y. -- Science. 2013 Feb 15;339(6121):780-5. doi: 10.1126/science.1228858. Epub 2013 Jan 3.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Institute of Meteoritics, University of New Mexico, Albuquerque, NM 87131, USA. agee@unm.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23287721" target="_blank"〉PubMed〈/a〉
    Keywords: Carbon/analysis ; Crystallization ; Iron/analysis ; Manganese/analysis ; *Mars ; *Meteoroids ; North America ; Oxygen Isotopes/analysis ; Radiometric Dating ; Water/analysis/*chemistry
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 6
    Publication Date: 2014-05-17
    Description: Because of differences in craniofacial morphology and dentition between the earliest American skeletons and modern Native Americans, separate origins have been postulated for them, despite genetic evidence to the contrary. We describe a near-complete human skeleton with an intact cranium and preserved DNA found with extinct fauna in a submerged cave on Mexico's Yucatan Peninsula. This skeleton dates to between 13,000 and 12,000 calendar years ago and has Paleoamerican craniofacial characteristics and a Beringian-derived mitochondrial DNA (mtDNA) haplogroup (D1). Thus, the differences between Paleoamericans and Native Americans probably resulted from in situ evolution rather than separate ancestry.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Chatters, James C -- Kennett, Douglas J -- Asmerom, Yemane -- Kemp, Brian M -- Polyak, Victor -- Blank, Alberto Nava -- Beddows, Patricia A -- Reinhardt, Eduard -- Arroyo-Cabrales, Joaquin -- Bolnick, Deborah A -- Malhi, Ripan S -- Culleton, Brendan J -- Erreguerena, Pilar Luna -- Rissolo, Dominique -- Morell-Hart, Shanti -- Stafford, Thomas W Jr -- New York, N.Y. -- Science. 2014 May 16;344(6185):750-4. doi: 10.1126/science.1252619.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Applied Paleoscience and DirectAMS, 10322 NE 190th Street, Bothell, WA 98011, USA. paleosci@gmail.com. ; Department of Anthropology and Institutes of Energy and the Environment, Pennsylvania State University, University Park, PA 16802, USA. ; Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131-0001, USA. ; Department of Anthropology and School of Biological Sciences, Washington State University, Pullman, WA 99164, USA. ; Bay Area Underwater Explorers, Berkeley, CA, USA. ; Department of Earth and Planetary Sciences, Northwestern University, Evanston, IL 60208, USA. ; School of Geography and Earth Sciences, McMaster University, Hamilton, Ontario L8S 4K1, Canada. ; Instituto Nacional Antropologia e Historia, Colonia Centro Historico, 06060, Mexico City, DF, Mexico. ; Department of Anthropology and Population Research Center, University of Texas at Austin, Austin, TX 78712, USA. ; Institute for Genomic Biology, University of Illinois, Urbana-Champaign, IL 61801, USA. ; Subdireccion de Arqueologia Subacuatica, Instituto Nacional de Antropologia e Historia, 06070 Mexico City, Mexico. ; Waitt Institute, La Jolla, CA 92038-1948, USA. ; Department of Anthropology, Stanford University, Stanford, CA 94305, USA. ; Centre for AMS C, Department of Physics and Astronomy, Aarhus University, Aarhus, Denmark, and Centre for GeoGenetics, Natural History Museum of Denmark, Geological Museum, Copenhagen, Denmark.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24833392" target="_blank"〉PubMed〈/a〉
    Keywords: Base Sequence ; *Biological Evolution ; DNA, Mitochondrial/genetics ; Haplotypes ; Humans ; Indians, North American/*genetics ; Mexico ; Molecular Sequence Data ; Paleontology ; Radiometric Dating ; *Skeleton ; Skull/anatomy & histology
    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: 2017-11-22
    Description: In carbonate terranes, rocks types that provide apatite are not available to effectively use apatite fission track (AFT) or (U/Th)-He chronometry (AHe). Here we suggest that calcite cave spar can be an effective chronometer and complimentary to AFT and AHe thermochronometers in carbonate regions such as our study area, the Guadalupe Mountains of southeastern New Mexico and west Texas. Our measured depth of cave spar deposition is 500 ± 250 meters beneath the regional water table, formed at temperatures of 40° to 80° C, indicating these caves and their spar crystals form near the supercritical CO 2 -subcritical CO 2 boundary where we interpret the origin of both the caves and spar to occur. This depth-temperature relationship suggests a higher than normal geotherm, likely associated with regional magmatic activity. As a case study we examined the timing of uplift of the Guadalupe Mountains previously attributed to the compressional Laramide orogeny (ca. 90 to 50 Ma), later extensional tectonics associated with Basin and Range (ca. 36 to 28 Ma) or the opening of the Rio Grande Rift (ca. 20 Ma to present). We show that most of the spar origin is coeval with the ignimbrite flare-up between 36 – 28 Ma. Our results constrain the initiation of Guadalupe Mountains block uplift, relative to the surrounding terrain, to between 27-16 Ma and reconstruct the evolution of a low-lying regional landscape prior to block uplift from 185 to 28 Ma, in support of models that attribute regional surface uplift to extensional tectonics and associated volcanism.
    Print ISSN: 0278-7407
    Electronic ISSN: 1944-9194
    Topics: Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 8
    Publication Date: 2013-06-25
    Description: In order to reconstruct the activity of the Indian Summer Monsoon (ISM) during the last ~4 kyr, two stalagmites from Baratang cave in Andaman Islands have been investigated for their temporal variations in δ 18 O. The chronology is provided by radiocarbon ages on the stalagmites. During 1800-2100 cal yr BP we observe a significant increase in stalagmite δ 18 O that we infer is caused by the amount effect. This increase implies a strong reduction in the strength of the ISM that is correlated with the Roman Warm Period. Other proxy records in the region confirm a reduction in ISM activity during this time. Reduction in the ISM is also observed around 1500 and 400-800 cal yr BP; the latter period is the transition from the Medieval Warm Period to the Little Ice Age. The strongest monsoon in the last ~4 kyr is observed during 800-1200 cal yr BP, the Medieval Warm Period.
    Electronic ISSN: 1525-2027
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 9
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 115 (1993), S. 245-256 
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 125 (1994), S. 235-254 
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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