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100   $a20111013d2011      uy             0
101 0 $aeng
135   $aur|n|---|||||
181   $ctxt
182   $cc
183   $acr
200 00$aTectonic, climatic, and cryospheric evolution of the Antarctic Peninsula$b[electronic resource] /$fJohn B. Anderson and Julia S. Wellner, editors
210   $aWashington, DC $cAmerican Geophysical Union$dc2011
215   $a1 online resource (225 p.)
225 0 $aSpecial publication ;$v63
300   $aDescription based upon print version of record.
311   $a1-299-70537-5 
311   $a0-87590-734-2 
320   $aIncludes bibliographical references and index.
327   $aTitle 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, Antarctica
327   $aHistory 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
330   $a Published by the American Geophysical Union as part of the Special Publications Series. Tectonic, Climatic, and Cryospheric Evolution of the Antarctic Peninsula presents the analysis of data collected during the SHALDRIL program, which sampled the most complete Cenozoic stratigraphic section in the Antarctic Peninsula. The stratigraphic intervals sampled fill major gaps in the existing stratigraphic record in the region, which is believed to have been the last place in Antarctica to become fully glaciated and, as such, the last refugium for plants and animals living on the 
410  0$aSpecial Publications
606   $aClimatic changes$zAntarctica
606   $aGeology$zAntarctica
606   $aGeology, Stratigraphic$yCenozoic
606   $aMorphotectonics$zAntarctica
607   $aAntarctica
615  0$aClimatic changes
615  0$aGeology
615  0$aGeology, Stratigraphic
615  0$aMorphotectonics
676   $a559.89
701   $aAnderson$b John B.$f1944-$0895688
701   $aWellner$b Julia S$0895689
712 02$aAmerican Geophysical Union.
801  0$bMiAaPQ
801  1$bMiAaPQ
801  2$bMiAaPQ
906   $aBOOK
912   $a996209524703316
996   $aTectonic, climatic, and cryospheric evolution of the Antarctic Peninsula$92000928
997   $aUNISA