Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7528
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dc.contributor.authorallPasschier, S.; Department of Earth and Environmental Studies, Montclair State University, Montclair, New Jersey 07043, USAen
dc.contributor.authorallBrowne, G.; GNS Science, PO Box 30-368, Lower Hutt 5040, New Zealanden
dc.contributor.authorallField, B.; GNS Science, PO Box 30-368, Lower Hutt 5040, New Zealanden
dc.contributor.authorallFielding, C. R.; Department of Earth and Atmospheric Sciences, University of Nebraska, Lincoln, Nebraska 68588, USAen
dc.contributor.authorallKrissek, L. A.; School of Earth Sciences, The Ohio State University, Columbus, Ohio 43210, USAen
dc.contributor.authorallPanter, K.; Department of Geology, Bowling Green State University, Bowling Green, Ohio 43403, USAen
dc.contributor.authorallPekar, S. F.; School of Earth and Environmental Sciences, Queens College, City University of New York, Flushing, New York 11367, USAen
dc.contributor.authorallANDRILL-SMS Science Team,; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.date.accessioned2012-01-24T14:18:47Zen
dc.date.available2012-01-24T14:18:47Zen
dc.date.issued2011-11en
dc.identifier.urihttp://hdl.handle.net/2122/7528en
dc.description.abstractIn 2007, the Antarctic Geological Drilling Program (ANDRILL) drilled 1138.54 m of strata ~10 km off the East Antarctic coast, includ ing an expanded early to middle Miocene succession not previously recovered from the Antarctic continental shelf. Here, we pre sent a facies model, distribution, and paleoclimatic interpretation for the AND-2A drill hole, which enable us, for the fi rst time, to reconstruct periods of early and middle Miocene glacial advance and retreat and paleo environmental changes at an ice-proximal site. Three types of facies associations can be recognized that imply signifi cantly different paleoclimatic interpretations. (1) A diamictite-dominated facies association represents glacially dominated depositional environments, including subglacial environments, with only brief intervals where ice-free coasts existed, and periods when the ice sheet was periodically larger than the modern ice sheet. (2) A stratified diamictite and mudstone facies association includes facies characteristic of open-marine to iceberg-infl uenced depositional environments and is more consistent with a very dynamic ice sheet, with a grounding line south of the modern position. (3) A mudstone-dominated facies association generally lacks diamictites and was produced in a glacially infl uenced hemipelagic depositional environment. Based on the distribution of these facies associations, we can conclude that the Antarctic ice sheets were dynamic, with grounding lines south of the modern location at ca. 20.1–19.6 Ma and ca. 19.3–18.7 Ma and during the Miocene climatic optimum, ca. 17.6–15.4 Ma, with ice-sheet and sea-ice minima at ca. 16.5–16.3 Ma and ca. 15.7–15.6 Ma. While glacial minima at ca. 20.1–19.6 Ma and ca. 19.3–18.7 Ma were characterized by temperate margins, an increased abundance of gravelly facies and diatomaceous siltstone and a lack of meltwater plume deposits suggest a cooler and drier climate with polythermal conditions for the Miocene climatic optimum (ca. 17.6–15.4 Ma). Several periods of major ice growth with a grounding line traversing the drill site are recognized between ca. 20.2 and 17.6 Ma, and after ca. 15.4 Ma, with evidence of cold polar glaciers with ice shelves. The AND-2A core provides proximal evidence that during the middle Miocene climate transition, an ice sheet larger than the modern ice sheet was already present by ca. 14.7 Ma, ~1 m.y. earlier than generally inferred from deep-sea oxygen isotope records. These fi ndings highlight the importance of high-latitude ice-proximal records for the interpretation of far-fi eld proxies across major climate transitions.en
dc.language.isoEnglishen
dc.publisher.nameGeological Society of Americaen
dc.relation.ispartofGSA Bulletinen
dc.relation.ispartofseries11-12 / 123 (2011)en
dc.subjectANDRILL-SMSen
dc.subjectMioceneen
dc.subjectRoss Seaen
dc.subjectAntarcticaen
dc.titleEarly and middle Miocene Antarctic glacial history from the sedimentary facies distribution in the AND-2A drill hole, Ross Sea, Antarcticaen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber2352-2365en
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatologyen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.10. Stratigraphyen
dc.subject.INGV04. Solid Earth::04.05. Geomagnetism::04.05.06. Paleomagnetismen
dc.identifier.doi10.1130/B30334.1en
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dc.description.obiettivoSpecifico1.8. Osservazioni di geofisica ambientaleen
dc.description.obiettivoSpecifico2.2. Laboratorio di paleomagnetismoen
dc.description.obiettivoSpecifico3.8. Geofisica per l'ambienteen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorPasschier, S.en
dc.contributor.authorBrowne, G.en
dc.contributor.authorField, B.en
dc.contributor.authorFielding, C. R.en
dc.contributor.authorKrissek, L. A.en
dc.contributor.authorPanter, K.en
dc.contributor.authorPekar, S. F.en
dc.contributor.authorANDRILL-SMS Science Team,en
dc.contributor.departmentDepartment of Earth and Environmental Studies, Montclair State University, Montclair, New Jersey 07043, USAen
dc.contributor.departmentGNS Science, PO Box 30-368, Lower Hutt 5040, New Zealanden
dc.contributor.departmentGNS Science, PO Box 30-368, Lower Hutt 5040, New Zealanden
dc.contributor.departmentDepartment of Earth and Atmospheric Sciences, University of Nebraska, Lincoln, Nebraska 68588, USAen
dc.contributor.departmentSchool of Earth Sciences, The Ohio State University, Columbus, Ohio 43210, USAen
dc.contributor.departmentDepartment of Geology, Bowling Green State University, Bowling Green, Ohio 43403, USAen
dc.contributor.departmentSchool of Earth and Environmental Sciences, Queens College, City University of New York, Flushing, New York 11367, USAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartment of Earth & Environmental Sciences, Montclair State University, 252 Mallory Hall, 1 Normal Avenue, Montclair, NJ 07043, USA-
crisitem.author.deptGNS Science, P.O. Box 30368, Lower Hutt, New Zealand-
crisitem.author.deptGNS Science-
crisitem.author.deptDepartment of Earth and Atmospheric Sciences, University of Nebraska, Lincoln, Nebraska 68588, USA-
crisitem.author.deptDept. of Geology, Bowling Green State University, Bowling Green, USA-
crisitem.author.deptSchool of Earth and Environmental Sciences, Queens College, City University of New York, Flushing, New York 11367, USA-
crisitem.author.dept0-
crisitem.author.orcid0000-0001-7204-7025-
crisitem.author.orcid0000-0002-2397-6116-
crisitem.author.orcid0000-0002-0990-5880-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
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