[meteorite-list] 3 INQUA abstracts re Younger Dryas cold era evidence, James P and Douglas J Kennett, July 2011 Bern, Switzerland: Rich Murray 2011.09.17
From: Rich Murray <rmforall_at_meteoritecentral.com>
Date: Sat, 17 Sep 2011 21:28:47 -0700 Message-ID: <CAHqJ8pZVEgTYDJH_WWL-asqBo7JiTeBsoVHv0taKq5xxAnmivA_at_mail.gmail.com> 3 INQUA abstracts re Younger Dryas cold era evidence, James P and Douglas J Kennett, July 2011 Bern, Switzerland: Rich Murray 2011.09.17 http://rmforall.blogspot.com/2011/09/3-inqua-abstracts-re-younger-dryas-cold.html http://cosmictusk.com/upcoming-bern-inqua-conference-packed-with-younger-dryas-boundary-studies [ Put the ID number in place of 1666 to get other abstracts ] http://www.inqua2011.ch/?a=programme&subnavi=abstract&id=1666&sessionid=60 Abstract ID: 1666 Title: Younger Dryas Onset Marked by Dramatic Environmental and Biotic Change Content: The onset of the Younger Dryas (YD) episode was marked by a complex array of abrupt and potentially linked changes in the Earth's environmental and biotic systems. We will broadly review YD changes in atmosphere and ocean circulation, ice sheets, North American continental hydrosphere, biosphere including extinctions, and human culture. The cause of the YD is controversial and currently debated, yet any causal hypothesis needs to account for these changes. YD cooling is enigmatic in its timing, magnitude and abruptness at near-peak insolation. Such cooling episodes with YD characteristics and timing in earlier Terminations appear more affiliated with terminal glacial episodes. YD onset is also outstanding because of close collective association with major, abrupt continental-scale ecological reorganization, megafaunal extinction and human adaptive shifts. The YD climate onset was remarkably abrupt (~one year) suggesting atmospheric climate response preceded oceanic change. Maximum cooling was atypically early, near the YD onset and associated with an abrupt increase in atmospheric dust. A major North American hydrographic reorganization, apparently associated with destabilization of ice sheet margins, was marked by abrupt switch in flow from the south to northern oceans. This outburst flooding may have coincided with major drainage of Lake Agassiz. Associated outburst floods affected widely separated areas of the Arctic. The ocean responded by major change in meridional overturning. On land, responses include widespread evidence of biomass burning; change in sediment deposition including a layer with exotic materials interpreted to be of cosmic impact origin; broad continental vegetation disruption; abrupt megafaunal extinction; and genetic bottlenecks reflecting population declines and/or animal migrations. The North American human record suggests abrupt disappearance of the Clovis culture; a human genetic bottleneck; and a widespread archeological gap during early YD centuries. Session: 60 The enigmatic Younger Dryas climatic episode Authors: James Kennett Presenter: James Kennett Type: oral ID: 1526 Title: Soot as Evidence for Widespread Fires at the Younger Dryas Onset (YDB, 12.9 ka) Content: Evidence continues to grow in support of a major extraterrestrial (ET) impact as a trigger for the late Pleistocene megafaunal extinction in North America at the onset of the Younger Dryas (YDB, 12.9 ka). Sediment at the base of a C-rich, dark layer is marked by peaks in magnetic microspherules, Ir, nanodiamonds, and other materials consistent with an ET event (Firestone, 2007; Kennett, 2008). This layer also exhibits spikes in charcoal, C spherules, glass-like C, and PAHs indicative of continent-wide burning, coeval with evidence for a major abrupt increase in burning in Greenland (Mayewski, 1993; Legrand, 1997). Synchronous, widespread soot in high abundances is a marker for extensive, impact-related fires. Soot analysis allowed us to test the possibility that the explosion of an impactor triggered combustion of biomass or fossil C, as hypothesized for the Cretaceous-Paleogene (K-P, 65 Ma) (Wolbach, 1985; Belcher et al., 2009). Previous analyses of samples from N. America and Europe, yielded YDB soot (? 10%) at two sites in N. America: Murray Springs, AZ (20 ppm) and Blackville, SC (2000 ppm) (Wolbach, 2007). We now report results from analysis of six more sites: Arlington Canyon and nearby Arlington Springs, CA; Bull Creek, OK; Hall's Cave, TX; Murray Springs (new sampling); and Lommel, Belgium. Soot concentrations spike in the YDB layer at four of these sites: 2000 ppm at Arlington Canyon, CA; 500 ppm at Bull Creek; 2000 ppm at Hall's Cave, TX; and 6000 ppm at Murray Springs, 30x higher than previously observed there. Significant YDB soot at five locations up to 3500 km apart across North America, combined with other wildfire evidence, suggests widespread burning and aeolian transport of soot across North America ~12.9 ka ago. These results support an impact sufficient to ignite continental-scale fires. Session: 60 The enigmatic Younger Dryas climatic episode Authors: Adrienne Stich Charles Kinzie James Kennett Allen West Wendy Wolbach Presenter: James Kennett Type: poster ID: 1584 Title: Human Population Decline across Parts of the Northern Hemisphere during the Younger Dryas Cooling Period Content: There is an ongoing debate about a possible human population decline or contraction at the onset of the Younger Dryas (YD) at 12.9 ka. We used three methods to test whether YD climate change affected human population levels. FREQUENCY ANALYSES. This method employed lithic projectile point data from the Paleoindian Database of the Americas (PIDBA, http://pidba.utk.edu ). We tallied diagnostic projectile points used by North American Paleoindian cultures, such as Clovis, that existed prior to about 12.9 ka, and obtained point totals that were larger than those of immediately post-Clovis cultures. For the SE U.S., the ratio of Clovis points (n=1993) to post-Clovis points (n=947) reveals a point decline of 52%. For the Great Plains, a comparison of Clovis and fluted points (n=4020) to Folsom points (n=2527) shows a point decline of 37%, suggesting a population contraction of similar magnitude. QUARRY USAGE. Eleven major Clovis-age lithic quarry sites in the Southeastern U.S. exhibit either limited usage or total abandonment just after the YD onset, only to resume normal usage hundreds of years later. Those usage patterns imply a severe population decline or reorganization around 12.9 ka. SUMMED PROBABILITIES. This method involved calibrating relevant 14C dates from across the Northern Hemisphere and combining the probabilities, after which major peaks and troughs in the trends were assumed to reflect changes in human demographics. We found an abrupt, statistically significant decline at 12.9 ka, followed by a rebound 200 to 900 years later. The overall decline was more than 50%, similar in magnitude to the decline in Clovis-Folsom point ratios. The coeval YD declines in projectile points, quarry usage, and 14C dates appear linked to significant changes in climate and biota. While the causes of the YD remain controversial, evidence suggests that human population declines occurred nearly simultaneously across the Northern Hemisphere around 12.9 ka. Session: 60 The enigmatic Younger Dryas climatic episode Authors: David G. Anderson Albert C. Goodyear James Kennett Allen West Presenter: James Kennett Type: poster http://www.geol.ucsb.edu/faculty/kennett/Home.html [ photo ] Professor: Marine Geology, Paleoceanography, Stratigraphy, Micropaleontology, Paleobiology Office: Webb Hall 1037A Phone: (805) 893-3103 or 805-893-4187 FAX: 805-893-2314 E-mail: kennett at geol.ucsb.edu Research Interests Research largely deals with earth system history during the Cenozoic based on the analyses of the deep sea sedimentary record and the uplifted marine record on land. A variety of paleoenvironmental proxies are used (stable isotopes, fossils, sediments) to reconstruct paleoclimatic, oceanographic and biotic changes in the sedimentary record. Of greatest interest is to help develop better understanding of past global changes; to evaluate the dynamic interactions that constantly occurred in the past between the several global spheres (lithosphere, oceansphere, atmosphere, cryosphere and biosphere). The kinds of questions we think about include the following: What is the climate evolution of the polar regions? When and how did the major ice sheets form? How have changes in ocean circulation affected global climate development? How did the oceans circulate during times of global warming? How tight are the linkages between climate change and thermohaline circulation? How rapidly do climate and oceans switch between different states and what processes drive these changes? How has the global climate changed during the classic ice-age period and how has this affected North American climate? What is the record of biological evolution in the oceans and how does this help with the understanding of evolutionary processes? Data related to this and other questions are generated in light stable isotope mass spectrometry and micropaleontological laboratories. http://pages.uoregon.edu/dkennett/ Department of Anthropology University of Oregon Eugene, OR 97403-1218 Phone (Office): 541-346-5106 E-mail: dkennett at uoregon.edu Abstracts for Session 60 ?The enigmatic Younger Dryas climatic episode? Oral Presentations July 20-27, 2011 INQUA Conference, Bern, Switzerland ID Title Presenter Talknbr. Invited 1666 Younger Dryas Onset Marked by Dramatic Environmental and Biotic Change James Kennett 1 x 835 The Younger-Dryas Cold reversal: Ice-Earth-Ocean Intercations During a Period of Rapid Climate Change Richard Peltier 2 x 366 Assessing the effectiveness of different freshwater drainage routes at triggering the Younger Dryas Alan Condron 3 2964 Reduced Atlantic Meridional Overturning Circulation (AMOC) and Regional Climate Change During the Younger Dryas Jerry McManus 4 x 3138 Oceanic Variability in the Gulf of Alaska during the Younger Dryas Summer K. Praetorius 5 1514 Abrupt changes in runoff from North America during the Younger Dryas James Teller 6 x 262 Younger Dryas glaciation of Scandinavia ? the type area for the Younger Dryas Jan Mangerud 7 x 1813 Unusual material in early Younger Dryas age sediments and their potential relevance to the YD Cosmic Impact Hypothesis Malcolm LeCompte 8 x 2641 Exceptional iridium concentrations found at the Aller?d-Younger Dryas transition in sediments from Bodmin Moor in southwest England William Marshall 9 1556 Nanodiamonds and the Usselo layer Annelies van Hoesel 10 2768 Vegetation change and the Younger Dryas: a continental-scale perspective Matthew Peros 11 x 209 The Younger Dryas in the Neotropics: paleoecological evidence from Venezuela Encarni Montoya 12 x Posters ID Title Presenter 583 New paleoclimatic reconstruction for the Aller?d and Young Dryas of the plain part of Ukraine (based on palynological data) Lyudmila Bezusko 997 Vegetation dynamics during Younger Dryas climatic episode (12600 ? 11500 yr. cal. B.P.) in Northwest Lithuania Eugenija Rudnickaite 1177 Effective moisture during the late glacial to Holocene transition from mainland eastern Australia John Tibby 1181 The boundary phenomenon of the Pleistocene ? Holocene in the Baikal Siberia (Russia) Natalia Berdnikova 1184 A review on the radiocarbon and absolute chronologies bracketing the Younger Dryas climatic event Edouard Bard 1294 Individual and community responses of diatoms to the Younger Dryas climatic reversal in a South Carpathian glacial lake Krisztina Buczk? 1378 North Atlantic reservoir ages linked to high Younger Dryas atmospheric radiocarbon concentrations William Austin 1447 The Bull Creek valley stream terraces, buried soils, and paleo-environment during the Younger Dryas in the Oklahoma Panhandle, USA Alexander Simms 1526 Soot as Evidence for Widespread Fires at the Younger Dryas Onset (YDB, 12.9 ka) James Kennett 1584 Human Population Decline across Parts of the Northern Hemisphere during the Younger Dryas Cooling Period James Kennett 1587 Eastward Drainage of Glacial Lake Agassiz: The Perspective from the Lake Superior Basin Steve M. Colman 1591 Nanodiamonds as Evidence for a Younger Dryas Cosmic Impact Event Allen West 1606 Shock-melt Evidence for a Cosmic Impact with Earth during the Younger Dryas at 12.9 ka Allen West 1619 Evidence for Widespread Biomass-Burning at the Younger Dryas Boundary at 12.9 ka Allen West 2667 Greater-than-present wet conditions from 14.6 to 10.2 cal ka yr BP in the southwestern Great Lakes area, North America Brandon Curry 2765 Evidence of Younger Dryas aridity in dune-paleosol successions in the Midwest of U.S.A. Hong Wang 2853 Pedogenic Climate Signals in the Great Plains (USA) during the Pleistocene-Holocene Transition (B?lling/Aller?d ? Boreal) William C Johnson 2875 The Aller?d-Younger Dryas Transition in lake sediments from The Netherlands Wim Hoek 3116 Megafaunal Extinction at the Younger Dryas Onset in North America Douglas Kennett 3134 Carolina Bays: Younger Dryas Time Capsules Malcolm LeCompte Pierson Barretto gives best amateur site for worldwide evidence for Holocene impacts: Rich Murray 2011.09.06 http://rmforall.blogspot.com/2011/09/pierson-barretto-gives-best-amateur.html www.cosmictusk.com blog for all point of view, now sharing major progress re mainstream research within mutual service, Rich Murray Rich Murray, MA Boston University Graduate School 1967 psychology, BS MIT 1964, history and physics, 1943 Otowi Road, Santa Fe, New Mexico 87505 rmforall at gmail.com 505-819-7388 Skype audio, video rich.murray11 http://RMForAll.blogspot.com new primary archive http://tech.groups.yahoo.com/group/AstroDeep/messages http://health.groups.yahoo.com/group/aspartameNM/messages group with 118 members, 1,625 posts in a public archive http://groups.yahoo.com/group/rmforall/messages ______________________________________________ Received on Sun 18 Sep 2011 12:28:47 AM PDT |
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