03758nam 2200721Ia 450 99620952470331620200520144314.01-118-66766-21-118-67241-01-118-67167-8(CKB)3370000000000508(EBL)1184589(OCoLC)843640347(SSID)ssj0000859871(PQKBManifestationID)11440992(PQKBTitleCode)TC0000859871(PQKBWorkID)10895320(PQKB)10754069(OCoLC)772505575(MiAaPQ)EBC1184589(Au-PeEL)EBL1184589(CaPaEBR)ebr10726742(CaONFJC)MIL501788(PPN)189610980(EXLCZ)99337000000000050820111013d2011 uy 0engur|n|---|||||txtccrTectonic, climatic, and cryospheric evolution of the Antarctic Peninsula[electronic resource] /John B. Anderson and Julia S. Wellner, editorsWashington, DC American Geophysical Unionc20111 online resource (225 p.)Special publication ;63Description based upon print version of record.1-299-70537-5 0-87590-734-2 Includes bibliographical references and index.Title Page; Contents; Preface; Introduction; A Different Look at Gateways: Drake Passage and Australia/Antarctica; Exhumational History of the Margins of Drake Passage From Thermochronology and Sediment Provenance; Seismic Stratigraphy of the Joinville Plateau: Implications for Regional Climate Evolution; Age Assessment of Eocene-Pliocene Drill Cores Recovered During the SHALDRIL II Expedition, Antarctic Peninsula; Magnetic Properties of Oligocene-Eocene Cores From SHALDRIL II, AntarcticaHistory of an Evolving Ice Sheet as Recorded in SHALDRIL Cores From the Northwestern Weddell Sea, AntarcticaCenozoic Glacial History of the Northern Antarctic Peninsula: A Micromorphological Investigation of Quartz Sand Grains; Last Remnants of Cenozoic Vegetation and Organic-Walled Phytoplankton in the Antarctic Peninsula's Icehouse World; Vegetation and Organic-Walled Phytoplankton at the End of the Antarctic Greenhouse World: Latest Eocene Cooling Events; AGU Category Index; Index Published by the American Geophysical Union as part of the Special Publications Series. Tectonic, Climatic, and Cryospheric Evolution of the Antarctic Peninsula presents the analysis of data collected during the SHALDRIL program, which sampled the most complete Cenozoic stratigraphic section in the Antarctic Peninsula. The stratigraphic intervals sampled fill major gaps in the existing stratigraphic record in the region, which is believed to have been the last place in Antarctica to become fully glaciated and, as such, the last refugium for plants and animals living on the Special PublicationsClimatic changesAntarcticaGeologyAntarcticaGeology, StratigraphicCenozoicMorphotectonicsAntarcticaAntarcticaClimatic changesGeologyGeology, StratigraphicMorphotectonics559.89Anderson John B.1944-895688Wellner Julia S895689American Geophysical Union.MiAaPQMiAaPQMiAaPQBOOK996209524703316Tectonic, climatic, and cryospheric evolution of the Antarctic Peninsula2000928UNISA