Glaciations in North and South America from the Miocene to the Last Glacial Maximum : Comparisons, Linkages and Uncertainties
Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to e...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Rutter, Nat [verfasserIn] |
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| Format: |
E-Book |
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| Sprache: |
Englisch |
| Erschienen: |
Dordrecht: Springer ; 2012 |
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| Schlagwörter: |
Amerika / Miozän / Pliozän / Pleistozän / Stratigraphie / Geologische Korrelation Südamerika / Neogen / Nordamerika / Formation, Geologie / Vereisung / Vereisung Amerika / Eiszeit / Vergletscherung / Glaziales Sediment / Gletschervorstoss Südamerika / Neogen / Nordamerika / Formation, Geologie / Vereisung Eiszeit / Vergletscherung / Glaziales Sediment / Gletschervorstoss |
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| Schlagwörter: |
| Anmerkung: |
Description based upon print version of record |
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| Umfang: |
Online-Ressource (XIII, 67 p. 18 illus., 13 illus. in color, digital) |
| Weitere Ausgabe: |
Buchausg. u.d.T.: Glaciations in North and South America from the Miocene to the Last Glacial Maximum - Dordrecht [u.a.] : Springer, 2012 |
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| Reihe: |
SpringerBriefs in Earth System Sciences SpringerLink ; Bücher |
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| Links: | |
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| ISBN: |
978-94-007-4399-1 |
| DOI / URN: |
10.1007/978-94-007-4399-1 |
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| Katalog-ID: |
1651541493 |
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| 245 | 1 | 0 | |a Glaciations in North and South America from the Miocene to the Last Glacial Maximum |b Comparisons, Linkages and Uncertainties |c by Nat Rutter, Andrea Coronato, Karin Helmens, Jorge Rabassa, Marcelo Zárate |
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| 505 | 8 | 0 | |a Glaciations in North and South America from the Miocene to the Last Glacial Maximum; Acknowledgments; Contents; Abstract; Introduction and Previous Work; 1 The Glacial and Loess Record of Southern South America; Abstract; Introduction; The Glacial Record; Glaciations During the Latest Miocene, Early Pliocene and Middle Pliocene (Gilbert Chron); Glaciations During the Late Pliocene (Gauss Chron); Glaciations During the Early Pleistocene (Matuyama Chron); The Great Patagonian Glaciation; Glaciations During the Middle-Late Pleistocene (Brunhes Chron) |
| 505 | 8 | 0 | |a The Late Pleistocene (Last Glacial Cycle: Brunhes Chron)The Loess Record; Miocene-Pliocene Loess (Gauss-Gilbert Chron); Pleistocene Loess (Brunhes-Matuyama-Gauss Chrons); Last Glacial Cycle (Brunhes Chron); References; 2 The Glacial Record of Northern South America; Abstract; Introduction; Glaciation During the Early Pleistocene (Matuyama Chron); Glaciation During the Middle-Late Pleistocene (Brunhes Chron); The Late Pleistocene (Last Glacial Cycle: Brunhes Chron); References; 3 The Glacial and Loess Record of North America; Abstract; Introduction; Mountain and Continental Glaciation |
| 505 | 8 | 0 | |a Glaciations During the Late Pliocene: Pleistocene (Gilbert and Gauss/Matuyama, and Matuyama Chrons)Glaciations During the Middle Pleistocene (Brunhes Chron); Glaciation During the Late Pleistocene (Brunhes Chron); The Loess Record; References; 4 Comparison of South and North American Glaciations; Abstract; Glaciations During the Miocene-Pliocene (Gilbert and Gauss Chrons) and Early Pleistocene (Matuyama Chron); Glaciations During the Middle and Late Pleistocene (Brunhes Chron); References; 5 Chinese Loess/Paleosol Record; Abstract; References; Discussion and Conclusions; References; |
| 520 | |a Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors | ||
| 520 | |a Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors. | ||
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Glaciations in North and South America from the Miocene to the Last Glacial Maximum; Acknowledgments; Contents; Abstract; Introduction and Previous Work; 1 The Glacial and Loess Record of Southern South America; Abstract; Introduction; The Glacial Record; Glaciations During the Latest Miocene, Early Pliocene and Middle Pliocene (Gilbert Chron); Glaciations During the Late Pliocene (Gauss Chron); Glaciations During the Early Pleistocene (Matuyama Chron); The Great Patagonian Glaciation; Glaciations During the Middle-Late Pleistocene (Brunhes Chron) The Late Pleistocene (Last Glacial Cycle: Brunhes Chron)The Loess Record; Miocene-Pliocene Loess (Gauss-Gilbert Chron); Pleistocene Loess (Brunhes-Matuyama-Gauss Chrons); Last Glacial Cycle (Brunhes Chron); References; 2 The Glacial Record of Northern South America; Abstract; Introduction; Glaciation During the Early Pleistocene (Matuyama Chron); Glaciation During the Middle-Late Pleistocene (Brunhes Chron); The Late Pleistocene (Last Glacial Cycle: Brunhes Chron); References; 3 The Glacial and Loess Record of North America; Abstract; Introduction; Mountain and Continental Glaciation Glaciations During the Late Pliocene: Pleistocene (Gilbert and Gauss/Matuyama, and Matuyama Chrons)Glaciations During the Middle Pleistocene (Brunhes Chron); Glaciation During the Late Pleistocene (Brunhes Chron); The Loess Record; References; 4 Comparison of South and North American Glaciations; Abstract; Glaciations During the Miocene-Pliocene (Gilbert and Gauss Chrons) and Early Pleistocene (Matuyama Chron); Glaciations During the Middle and Late Pleistocene (Brunhes Chron); References; 5 Chinese Loess/Paleosol Record; Abstract; References; Discussion and Conclusions; References; |
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Glaciations in North and South America from the Miocene to the Last Glacial Maximum; Acknowledgments; Contents; Abstract; Introduction and Previous Work; 1 The Glacial and Loess Record of Southern South America; Abstract; Introduction; The Glacial Record; Glaciations During the Latest Miocene, Early Pliocene and Middle Pliocene (Gilbert Chron); Glaciations During the Late Pliocene (Gauss Chron); Glaciations During the Early Pleistocene (Matuyama Chron); The Great Patagonian Glaciation; Glaciations During the Middle-Late Pleistocene (Brunhes Chron) The Late Pleistocene (Last Glacial Cycle: Brunhes Chron)The Loess Record; Miocene-Pliocene Loess (Gauss-Gilbert Chron); Pleistocene Loess (Brunhes-Matuyama-Gauss Chrons); Last Glacial Cycle (Brunhes Chron); References; 2 The Glacial Record of Northern South America; Abstract; Introduction; Glaciation During the Early Pleistocene (Matuyama Chron); Glaciation During the Middle-Late Pleistocene (Brunhes Chron); The Late Pleistocene (Last Glacial Cycle: Brunhes Chron); References; 3 The Glacial and Loess Record of North America; Abstract; Introduction; Mountain and Continental Glaciation Glaciations During the Late Pliocene: Pleistocene (Gilbert and Gauss/Matuyama, and Matuyama Chrons)Glaciations During the Middle Pleistocene (Brunhes Chron); Glaciation During the Late Pleistocene (Brunhes Chron); The Loess Record; References; 4 Comparison of South and North American Glaciations; Abstract; Glaciations During the Miocene-Pliocene (Gilbert and Gauss Chrons) and Early Pleistocene (Matuyama Chron); Glaciations During the Middle and Late Pleistocene (Brunhes Chron); References; 5 Chinese Loess/Paleosol Record; Abstract; References; Discussion and Conclusions; References; Rutter, Nat misc QE1-996.5 misc Geography misc Geology misc Paleontology misc Climatic changes misc Earth Sciences gnd Amerika gnd Miozän gnd Pliozän gnd Pleistozän gnd Stratigraphie gnd Geologische Korrelation gnd Südamerika gnd Neogen gnd Nordamerika gnd Formation gnd Vereisung gnd Eiszeit gnd Vergletscherung gnd Glaziales Sediment gnd Gletschervorstoss 2027 ebook Glaciations in North and South America from the Miocene to the Last Glacial Maximum Comparisons, Linkages and Uncertainties |
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Glaciations in North and South America from the Miocene to the Last Glacial Maximum Comparisons, Linkages and Uncertainties |
| abstract |
Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors. Description based upon print version of record |
| abstractGer |
Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors. Description based upon print version of record |
| abstract_unstemmed |
Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors. Description based upon print version of record |
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9789400743991 978-94-007-4399-1 10.1007/978-94-007-4399-1 doi (DE-627)1651541493 (DE-576)36768859X (DE-599)BSZ36768859X (OCoLC)840011289 (OCoLC)840011289 (DE-He213)978-94-007-4399-1 DE-627 ger DE-627 rakwb eng XA-NL QE1-996.5 RBG bicssc SCI031000 bisacsh Rutter, Nat verfasserin aut Glaciations in North and South America from the Miocene to the Last Glacial Maximum Comparisons, Linkages and Uncertainties by Nat Rutter, Andrea Coronato, Karin Helmens, Jorge Rabassa, Marcelo Zárate Dordrecht Springer 2012 Online-Ressource (XIII, 67 p. 18 illus., 13 illus. in color, digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier SpringerBriefs in Earth System Sciences SpringerLink Bücher Description based upon print version of record Glaciations in North and South America from the Miocene to the Last Glacial Maximum; Acknowledgments; Contents; Abstract; Introduction and Previous Work; 1 The Glacial and Loess Record of Southern South America; Abstract; Introduction; The Glacial Record; Glaciations During the Latest Miocene, Early Pliocene and Middle Pliocene (Gilbert Chron); Glaciations During the Late Pliocene (Gauss Chron); Glaciations During the Early Pleistocene (Matuyama Chron); The Great Patagonian Glaciation; Glaciations During the Middle-Late Pleistocene (Brunhes Chron) The Late Pleistocene (Last Glacial Cycle: Brunhes Chron)The Loess Record; Miocene-Pliocene Loess (Gauss-Gilbert Chron); Pleistocene Loess (Brunhes-Matuyama-Gauss Chrons); Last Glacial Cycle (Brunhes Chron); References; 2 The Glacial Record of Northern South America; Abstract; Introduction; Glaciation During the Early Pleistocene (Matuyama Chron); Glaciation During the Middle-Late Pleistocene (Brunhes Chron); The Late Pleistocene (Last Glacial Cycle: Brunhes Chron); References; 3 The Glacial and Loess Record of North America; Abstract; Introduction; Mountain and Continental Glaciation Glaciations During the Late Pliocene: Pleistocene (Gilbert and Gauss/Matuyama, and Matuyama Chrons)Glaciations During the Middle Pleistocene (Brunhes Chron); Glaciation During the Late Pleistocene (Brunhes Chron); The Loess Record; References; 4 Comparison of South and North American Glaciations; Abstract; Glaciations During the Miocene-Pliocene (Gilbert and Gauss Chrons) and Early Pleistocene (Matuyama Chron); Glaciations During the Middle and Late Pleistocene (Brunhes Chron); References; 5 Chinese Loess/Paleosol Record; Abstract; References; Discussion and Conclusions; References; Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors. 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Glaciations in North and South America from the Miocene to the Last Glacial Maximum Dordrecht [u.a.] : Springer, 2012 XIII, 67 S. 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Kein systematisches Downloaden durch Robots. i z 03-09-12 2027 01 DE-105 3350045561 00 --%%-- --%%-- n --%%-- Campuslizenz l01 29-06-12 2050 01 DE-Zi4 3350045596 00 --%%-- --%%-- n --%%-- Elektronischer Volltext - Campuslizenz l01 29-06-12 2061 01 DE-520 3350045618 00 --%%-- --%%-- n --%%-- eBook, Link nur im Campusbereich nutzbar l01 29-06-12 2148 01 DE-950 3350045634 00 --%%-- eBook Springer --%%-- n Elektronischer Volltext - Campuslizenz l01 04-07-12 22 01 0018 Volltextzugang Campus https://doi.org/10.1007/978-94-007-4399-1 22 01 0018 Nur für Angehörige der Universität Hamburg: Volltextzugang von außerhalb des Campus http://emedien.sub.uni-hamburg.de/han/SpringerEbooks/doi.org/10.1007/978-94-007-4399-1 40 01 0007 Volltext, Campuszugriff http://dx.doi.org/10.1007/978-94-007-4399-1 40 01 0007 Volltext, Externer Zugriff http://han.sub.uni-goettingen.de/han/Springer-eBook-EarthEnvironmentalScience/dx.doi.org/10.1007/978-94-007-4399-1 40 01 0007 Dieser Titel ist Teil einer Datenbank http://www.bibliothek.uni-regensburg.de/dbinfo/frontdoor.php?titel_id=10159&bibid=SUBGO 60 01 0705 Volltextzugang Campus https://doi.org/10.1007/978-94-007-4399-1 62 01 0028 https://doi.org/10.1007/978-94-007-4399-1 65 01 0003 Volltextzugang Campus https://doi.org/10.1007/978-94-007-4399-1 110 01 3110 https://doi.org/10.1007/978-94-007-4399-1 120 01 0715 http://dx.doi.org/10.1007/978-94-007-4399-1 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991016132185203501 120 03 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991016132185203501 285 01 0517 E-books (Springer) https://doi.org/10.1007/978-94-007-4399-1 370 01 4370 E-Book: Zugriff im HCU-Netz. 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9789400743991 978-94-007-4399-1 10.1007/978-94-007-4399-1 doi (DE-627)1651541493 (DE-576)36768859X (DE-599)BSZ36768859X (OCoLC)840011289 (OCoLC)840011289 (DE-He213)978-94-007-4399-1 DE-627 ger DE-627 rakwb eng XA-NL QE1-996.5 RBG bicssc SCI031000 bisacsh Rutter, Nat verfasserin aut Glaciations in North and South America from the Miocene to the Last Glacial Maximum Comparisons, Linkages and Uncertainties by Nat Rutter, Andrea Coronato, Karin Helmens, Jorge Rabassa, Marcelo Zárate Dordrecht Springer 2012 Online-Ressource (XIII, 67 p. 18 illus., 13 illus. in color, digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier SpringerBriefs in Earth System Sciences SpringerLink Bücher Description based upon print version of record Glaciations in North and South America from the Miocene to the Last Glacial Maximum; Acknowledgments; Contents; Abstract; Introduction and Previous Work; 1 The Glacial and Loess Record of Southern South America; Abstract; Introduction; The Glacial Record; Glaciations During the Latest Miocene, Early Pliocene and Middle Pliocene (Gilbert Chron); Glaciations During the Late Pliocene (Gauss Chron); Glaciations During the Early Pleistocene (Matuyama Chron); The Great Patagonian Glaciation; Glaciations During the Middle-Late Pleistocene (Brunhes Chron) The Late Pleistocene (Last Glacial Cycle: Brunhes Chron)The Loess Record; Miocene-Pliocene Loess (Gauss-Gilbert Chron); Pleistocene Loess (Brunhes-Matuyama-Gauss Chrons); Last Glacial Cycle (Brunhes Chron); References; 2 The Glacial Record of Northern South America; Abstract; Introduction; Glaciation During the Early Pleistocene (Matuyama Chron); Glaciation During the Middle-Late Pleistocene (Brunhes Chron); The Late Pleistocene (Last Glacial Cycle: Brunhes Chron); References; 3 The Glacial and Loess Record of North America; Abstract; Introduction; Mountain and Continental Glaciation Glaciations During the Late Pliocene: Pleistocene (Gilbert and Gauss/Matuyama, and Matuyama Chrons)Glaciations During the Middle Pleistocene (Brunhes Chron); Glaciation During the Late Pleistocene (Brunhes Chron); The Loess Record; References; 4 Comparison of South and North American Glaciations; Abstract; Glaciations During the Miocene-Pliocene (Gilbert and Gauss Chrons) and Early Pleistocene (Matuyama Chron); Glaciations During the Middle and Late Pleistocene (Brunhes Chron); References; 5 Chinese Loess/Paleosol Record; Abstract; References; Discussion and Conclusions; References; Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors. 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Glaciations in North and South America from the Miocene to the Last Glacial Maximum Dordrecht [u.a.] : Springer, 2012 XIII, 67 S. (DE-627)1616050004 (DE-576)362370281 9789400743984 https://doi.org/10.1007/978-94-007-4399-1 Verlag Volltext http://dx.doi.org/10.1007/978-94-007-4399-1 Resolving-System lizenzpflichtig Volltext https://swbplus.bsz-bw.de/bsz36768859xcov.jpg V:DE-576 X:springer image/jpeg 20140213092307 Cover https://swbplus.bsz-bw.de/bsz362370281inh.htm V:DE-576;B:DE-105 application/pdf 20120904105816 Inhaltsverzeichnis (DE-627)718778448 ZDB-2-EES 2012 GBV_ILN_22 ISIL_DE-18 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_22_i05715 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_62 ISIL_DE-28 GBV_ILN_65 ISIL_DE-3 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_120 ISIL_DE-715 GBV_ILN_285 ISIL_DE-517 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2061 ISIL_DE-520 GBV_ILN_2148 ISIL_DE-950 GBV ExPruef BO 045F 551 045F 551.7/92 22 01 0018 1314928295 00 --%%-- --%%-- s --%%-- h57-ees Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. zi05715 29-07-12 40 01 0007 1340084570 OLR-SPRINGER-EES nl xsn 21-11-12 60 01 0705 4304956582 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 62 01 0028 1315016974 OLR-SEB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. 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Kein systematisches Downloaden. z 15-03-13 120 02 0715 3577176105 00 --%%-- --%%-- g --%%-- alma ww z 20-01-20 120 03 0715 1752703995 00 --%%-- --%%-- g --%%-- alma ww z 22-02-18 285 01 0517 1449601979 00 --%%-- --%%-- s --%%-- OLR-ESP-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. z 09-12-13 370 01 4370 1324405422 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 03-09-12 2027 01 DE-105 3350045561 00 --%%-- --%%-- n --%%-- Campuslizenz l01 29-06-12 2050 01 DE-Zi4 3350045596 00 --%%-- --%%-- n --%%-- Elektronischer Volltext - Campuslizenz l01 29-06-12 2061 01 DE-520 3350045618 00 --%%-- --%%-- n --%%-- eBook, Link nur im Campusbereich nutzbar l01 29-06-12 2148 01 DE-950 3350045634 00 --%%-- eBook Springer --%%-- n Elektronischer Volltext - Campuslizenz l01 04-07-12 22 01 0018 Volltextzugang Campus https://doi.org/10.1007/978-94-007-4399-1 22 01 0018 Nur für Angehörige der Universität Hamburg: Volltextzugang von außerhalb des Campus http://emedien.sub.uni-hamburg.de/han/SpringerEbooks/doi.org/10.1007/978-94-007-4399-1 40 01 0007 Volltext, Campuszugriff http://dx.doi.org/10.1007/978-94-007-4399-1 40 01 0007 Volltext, Externer Zugriff http://han.sub.uni-goettingen.de/han/Springer-eBook-EarthEnvironmentalScience/dx.doi.org/10.1007/978-94-007-4399-1 40 01 0007 Dieser Titel ist Teil einer Datenbank http://www.bibliothek.uni-regensburg.de/dbinfo/frontdoor.php?titel_id=10159&bibid=SUBGO 60 01 0705 Volltextzugang Campus https://doi.org/10.1007/978-94-007-4399-1 62 01 0028 https://doi.org/10.1007/978-94-007-4399-1 65 01 0003 Volltextzugang Campus https://doi.org/10.1007/978-94-007-4399-1 110 01 3110 https://doi.org/10.1007/978-94-007-4399-1 120 01 0715 http://dx.doi.org/10.1007/978-94-007-4399-1 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991016132185203501 120 03 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991016132185203501 285 01 0517 E-books (Springer) https://doi.org/10.1007/978-94-007-4399-1 370 01 4370 E-Book: Zugriff im HCU-Netz. 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9789400743991 978-94-007-4399-1 10.1007/978-94-007-4399-1 doi (DE-627)1651541493 (DE-576)36768859X (DE-599)BSZ36768859X (OCoLC)840011289 (OCoLC)840011289 (DE-He213)978-94-007-4399-1 DE-627 ger DE-627 rakwb eng XA-NL QE1-996.5 RBG bicssc SCI031000 bisacsh Rutter, Nat verfasserin aut Glaciations in North and South America from the Miocene to the Last Glacial Maximum Comparisons, Linkages and Uncertainties by Nat Rutter, Andrea Coronato, Karin Helmens, Jorge Rabassa, Marcelo Zárate Dordrecht Springer 2012 Online-Ressource (XIII, 67 p. 18 illus., 13 illus. in color, digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier SpringerBriefs in Earth System Sciences SpringerLink Bücher Description based upon print version of record Glaciations in North and South America from the Miocene to the Last Glacial Maximum; Acknowledgments; Contents; Abstract; Introduction and Previous Work; 1 The Glacial and Loess Record of Southern South America; Abstract; Introduction; The Glacial Record; Glaciations During the Latest Miocene, Early Pliocene and Middle Pliocene (Gilbert Chron); Glaciations During the Late Pliocene (Gauss Chron); Glaciations During the Early Pleistocene (Matuyama Chron); The Great Patagonian Glaciation; Glaciations During the Middle-Late Pleistocene (Brunhes Chron) The Late Pleistocene (Last Glacial Cycle: Brunhes Chron)The Loess Record; Miocene-Pliocene Loess (Gauss-Gilbert Chron); Pleistocene Loess (Brunhes-Matuyama-Gauss Chrons); Last Glacial Cycle (Brunhes Chron); References; 2 The Glacial Record of Northern South America; Abstract; Introduction; Glaciation During the Early Pleistocene (Matuyama Chron); Glaciation During the Middle-Late Pleistocene (Brunhes Chron); The Late Pleistocene (Last Glacial Cycle: Brunhes Chron); References; 3 The Glacial and Loess Record of North America; Abstract; Introduction; Mountain and Continental Glaciation Glaciations During the Late Pliocene: Pleistocene (Gilbert and Gauss/Matuyama, and Matuyama Chrons)Glaciations During the Middle Pleistocene (Brunhes Chron); Glaciation During the Late Pleistocene (Brunhes Chron); The Loess Record; References; 4 Comparison of South and North American Glaciations; Abstract; Glaciations During the Miocene-Pliocene (Gilbert and Gauss Chrons) and Early Pleistocene (Matuyama Chron); Glaciations During the Middle and Late Pleistocene (Brunhes Chron); References; 5 Chinese Loess/Paleosol Record; Abstract; References; Discussion and Conclusions; References; Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors. 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Glaciations in North and South America from the Miocene to the Last Glacial Maximum Dordrecht [u.a.] : Springer, 2012 XIII, 67 S. (DE-627)1616050004 (DE-576)362370281 9789400743984 https://doi.org/10.1007/978-94-007-4399-1 Verlag Volltext http://dx.doi.org/10.1007/978-94-007-4399-1 Resolving-System lizenzpflichtig Volltext https://swbplus.bsz-bw.de/bsz36768859xcov.jpg V:DE-576 X:springer image/jpeg 20140213092307 Cover https://swbplus.bsz-bw.de/bsz362370281inh.htm V:DE-576;B:DE-105 application/pdf 20120904105816 Inhaltsverzeichnis (DE-627)718778448 ZDB-2-EES 2012 GBV_ILN_22 ISIL_DE-18 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_22_i05715 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_62 ISIL_DE-28 GBV_ILN_65 ISIL_DE-3 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_120 ISIL_DE-715 GBV_ILN_285 ISIL_DE-517 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2061 ISIL_DE-520 GBV_ILN_2148 ISIL_DE-950 GBV ExPruef BO 045F 551 045F 551.7/92 22 01 0018 1314928295 00 --%%-- --%%-- s --%%-- h57-ees Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. zi05715 29-07-12 40 01 0007 1340084570 OLR-SPRINGER-EES nl xsn 21-11-12 60 01 0705 4304956582 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 62 01 0028 1315016974 OLR-SEB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. 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9789400743991 978-94-007-4399-1 10.1007/978-94-007-4399-1 doi (DE-627)1651541493 (DE-576)36768859X (DE-599)BSZ36768859X (OCoLC)840011289 (OCoLC)840011289 (DE-He213)978-94-007-4399-1 DE-627 ger DE-627 rakwb eng XA-NL QE1-996.5 RBG bicssc SCI031000 bisacsh Rutter, Nat verfasserin aut Glaciations in North and South America from the Miocene to the Last Glacial Maximum Comparisons, Linkages and Uncertainties by Nat Rutter, Andrea Coronato, Karin Helmens, Jorge Rabassa, Marcelo Zárate Dordrecht Springer 2012 Online-Ressource (XIII, 67 p. 18 illus., 13 illus. in color, digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier SpringerBriefs in Earth System Sciences SpringerLink Bücher Description based upon print version of record Glaciations in North and South America from the Miocene to the Last Glacial Maximum; Acknowledgments; Contents; Abstract; Introduction and Previous Work; 1 The Glacial and Loess Record of Southern South America; Abstract; Introduction; The Glacial Record; Glaciations During the Latest Miocene, Early Pliocene and Middle Pliocene (Gilbert Chron); Glaciations During the Late Pliocene (Gauss Chron); Glaciations During the Early Pleistocene (Matuyama Chron); The Great Patagonian Glaciation; Glaciations During the Middle-Late Pleistocene (Brunhes Chron) The Late Pleistocene (Last Glacial Cycle: Brunhes Chron)The Loess Record; Miocene-Pliocene Loess (Gauss-Gilbert Chron); Pleistocene Loess (Brunhes-Matuyama-Gauss Chrons); Last Glacial Cycle (Brunhes Chron); References; 2 The Glacial Record of Northern South America; Abstract; Introduction; Glaciation During the Early Pleistocene (Matuyama Chron); Glaciation During the Middle-Late Pleistocene (Brunhes Chron); The Late Pleistocene (Last Glacial Cycle: Brunhes Chron); References; 3 The Glacial and Loess Record of North America; Abstract; Introduction; Mountain and Continental Glaciation Glaciations During the Late Pliocene: Pleistocene (Gilbert and Gauss/Matuyama, and Matuyama Chrons)Glaciations During the Middle Pleistocene (Brunhes Chron); Glaciation During the Late Pleistocene (Brunhes Chron); The Loess Record; References; 4 Comparison of South and North American Glaciations; Abstract; Glaciations During the Miocene-Pliocene (Gilbert and Gauss Chrons) and Early Pleistocene (Matuyama Chron); Glaciations During the Middle and Late Pleistocene (Brunhes Chron); References; 5 Chinese Loess/Paleosol Record; Abstract; References; Discussion and Conclusions; References; Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors. Geography Geology Paleontology Climatic changes Earth Sciences Geography Geology Paleontology Climatic changes g (DE-588)4001670-5 (DE-627)106396161 (DE-576)208843884 Amerika gnd s (DE-588)4039517-0 (DE-627)106227793 (DE-576)209035293 Miozän gnd s (DE-588)4174919-4 (DE-627)104261765 (DE-576)20996006X Pliozän gnd s (DE-588)4046350-3 (DE-627)106198378 (DE-576)209069120 Pleistozän gnd s (DE-588)4057956-6 (DE-627)104459107 (DE-576)209124229 Stratigraphie gnd s (DE-588)4156695-6 (DE-627)104548215 (DE-576)209828803 Geologische Korrelation gnd (DE-627) g (DE-588)4078014-4 (DE-627)106078712 (DE-576)209206950 Südamerika gnd s (DE-588)4130779-3 (DE-627)105699934 (DE-576)209621877 Neogen gnd g (DE-588)4042483-2 (DE-627)106214179 (DE-576)209050675 Nordamerika gnd s (DE-588)4155003-1 (DE-627)104399694 (DE-576)209815523 Formation Geologie gnd s (DE-588)4187665-9 (DE-627)105270423 (DE-576)210047275 Vereisung gnd s (DE-588)4187665-9 (DE-627)105270423 (DE-576)210047275 Vereisung gnd (DE-627) g (DE-588)4001670-5 (DE-627)106396161 (DE-576)208843884 Amerika gnd s (DE-588)4014129-9 (DE-627)10634109X (DE-576)208906614 Eiszeit gnd s (DE-588)4187746-9 (DE-627)104160608 (DE-576)210047895 Vergletscherung gnd s (DE-588)4157505-2 (DE-627)105500305 (DE-576)209835044 Glaziales Sediment gnd s (DE-588)4396776-0 (DE-627)191531812 (DE-576)212004212 Gletschervorstoss gnd (DE-627) g (DE-588)4001670-5 (DE-627)106396161 (DE-576)208843884 Amerika gnd s (DE-588)4039517-0 (DE-627)106227793 (DE-576)209035293 Miozän gnd s (DE-588)4174919-4 (DE-627)104261765 (DE-576)20996006X Pliozän gnd s (DE-588)4046350-3 (DE-627)106198378 (DE-576)209069120 Pleistozän gnd s (DE-588)4057956-6 (DE-627)104459107 (DE-576)209124229 Stratigraphie gnd s (DE-588)4156695-6 (DE-627)104548215 (DE-576)209828803 Geologische Korrelation gnd (DE-627) g (DE-588)4078014-4 (DE-627)106078712 (DE-576)209206950 Südamerika gnd s (DE-588)4130779-3 (DE-627)105699934 (DE-576)209621877 Neogen gnd g (DE-588)4042483-2 (DE-627)106214179 (DE-576)209050675 Nordamerika gnd s (DE-588)4155003-1 (DE-627)104399694 (DE-576)209815523 Formation Geologie gnd s (DE-588)4187665-9 (DE-627)105270423 (DE-576)210047275 Vereisung gnd (DE-627) s (DE-588)4014129-9 (DE-627)10634109X (DE-576)208906614 Eiszeit gnd s (DE-588)4187746-9 (DE-627)104160608 (DE-576)210047895 Vergletscherung gnd s (DE-588)4157505-2 (DE-627)105500305 (DE-576)209835044 Glaziales Sediment gnd s (DE-588)4396776-0 (DE-627)191531812 (DE-576)212004212 Gletschervorstoss gnd (DE-627) Coronato, Andrea oth Helmens, Karin oth Rabassa, Jorge oth Zárate, Marcelo (DE-588)172553660 (DE-627)697489485 (DE-576)133413616 oth 9789400743984 Buchausg. u.d.T. Glaciations in North and South America from the Miocene to the Last Glacial Maximum Dordrecht [u.a.] : Springer, 2012 XIII, 67 S. 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Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. zi05715 29-07-12 40 01 0007 1340084570 OLR-SPRINGER-EES nl xsn 21-11-12 60 01 0705 4304956582 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 62 01 0028 1315016974 OLR-SEB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. 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9789400743991 978-94-007-4399-1 10.1007/978-94-007-4399-1 doi (DE-627)1651541493 (DE-576)36768859X (DE-599)BSZ36768859X (OCoLC)840011289 (OCoLC)840011289 (DE-He213)978-94-007-4399-1 DE-627 ger DE-627 rakwb eng XA-NL QE1-996.5 RBG bicssc SCI031000 bisacsh Rutter, Nat verfasserin aut Glaciations in North and South America from the Miocene to the Last Glacial Maximum Comparisons, Linkages and Uncertainties by Nat Rutter, Andrea Coronato, Karin Helmens, Jorge Rabassa, Marcelo Zárate Dordrecht Springer 2012 Online-Ressource (XIII, 67 p. 18 illus., 13 illus. in color, digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier SpringerBriefs in Earth System Sciences SpringerLink Bücher Description based upon print version of record Glaciations in North and South America from the Miocene to the Last Glacial Maximum; Acknowledgments; Contents; Abstract; Introduction and Previous Work; 1 The Glacial and Loess Record of Southern South America; Abstract; Introduction; The Glacial Record; Glaciations During the Latest Miocene, Early Pliocene and Middle Pliocene (Gilbert Chron); Glaciations During the Late Pliocene (Gauss Chron); Glaciations During the Early Pleistocene (Matuyama Chron); The Great Patagonian Glaciation; Glaciations During the Middle-Late Pleistocene (Brunhes Chron) The Late Pleistocene (Last Glacial Cycle: Brunhes Chron)The Loess Record; Miocene-Pliocene Loess (Gauss-Gilbert Chron); Pleistocene Loess (Brunhes-Matuyama-Gauss Chrons); Last Glacial Cycle (Brunhes Chron); References; 2 The Glacial Record of Northern South America; Abstract; Introduction; Glaciation During the Early Pleistocene (Matuyama Chron); Glaciation During the Middle-Late Pleistocene (Brunhes Chron); The Late Pleistocene (Last Glacial Cycle: Brunhes Chron); References; 3 The Glacial and Loess Record of North America; Abstract; Introduction; Mountain and Continental Glaciation Glaciations During the Late Pliocene: Pleistocene (Gilbert and Gauss/Matuyama, and Matuyama Chrons)Glaciations During the Middle Pleistocene (Brunhes Chron); Glaciation During the Late Pleistocene (Brunhes Chron); The Loess Record; References; 4 Comparison of South and North American Glaciations; Abstract; Glaciations During the Miocene-Pliocene (Gilbert and Gauss Chrons) and Early Pleistocene (Matuyama Chron); Glaciations During the Middle and Late Pleistocene (Brunhes Chron); References; 5 Chinese Loess/Paleosol Record; Abstract; References; Discussion and Conclusions; References; Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors. 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Glaciations in North and South America from the Miocene to the Last Glacial Maximum Dordrecht [u.a.] : Springer, 2012 XIII, 67 S. 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Neue Welt America Westliche Hemisphäre Amerika Miozän Pliozän Eiszeitalter Diluvium Eiszeit <Quartär> Pleistozän Schichtenkunde Stratigraphie Stratigraphische Korrelation Geologische Korrelation Amerika (Süd) Ameryka Południowa Südamerika Jungtertiär Spättertiär Neogen Amerika (Nord) Nordamerika Geologische Formation System <Stratigraphie> Formation <Geologie> Vereisung Kaltzeit Eiszeiten Glazialperiode Eiszeit Vergletscherung Glazialsediment Glaziales Sediment Gletscher / Wachstum Gletscherwachstum Gletschervorstoss Zárate, Marcelo A. Zárate, M. A. Zárate, Marcelo |
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Acknowledgments; Contents; Abstract; Introduction and Previous Work; 1 The Glacial and Loess Record of Southern South America; Abstract; Introduction; The Glacial Record; Glaciations During the Latest Miocene, Early Pliocene and Middle Pliocene (Gilbert Chron); Glaciations During the Late Pliocene (Gauss Chron); Glaciations During the Early Pleistocene (Matuyama Chron); The Great Patagonian Glaciation; Glaciations During the Middle-Late Pleistocene (Brunhes Chron)</subfield></datafield><datafield tag="505" ind1="8" ind2="0"><subfield code="a">The Late Pleistocene (Last Glacial Cycle: Brunhes Chron)The Loess Record; Miocene-Pliocene Loess (Gauss-Gilbert Chron); Pleistocene Loess (Brunhes-Matuyama-Gauss Chrons); Last Glacial Cycle (Brunhes Chron); References; 2 The Glacial Record of Northern South America; Abstract; Introduction; Glaciation During the Early Pleistocene (Matuyama Chron); Glaciation During the Middle-Late Pleistocene (Brunhes Chron); The Late Pleistocene (Last Glacial Cycle: Brunhes Chron); References; 3 The Glacial and Loess Record of North America; Abstract; Introduction; Mountain and Continental Glaciation</subfield></datafield><datafield tag="505" ind1="8" ind2="0"><subfield code="a">Glaciations During the Late Pliocene: Pleistocene (Gilbert and Gauss/Matuyama, and Matuyama Chrons)Glaciations During the Middle Pleistocene (Brunhes Chron); Glaciation During the Late Pleistocene (Brunhes Chron); The Loess Record; References; 4 Comparison of South and North American Glaciations; Abstract; Glaciations During the Miocene-Pliocene (Gilbert and Gauss Chrons) and Early Pleistocene (Matuyama Chron); Glaciations During the Middle and Late Pleistocene (Brunhes Chron); References; 5 Chinese Loess/Paleosol Record; Abstract; References; Discussion and Conclusions; References;</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors.</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Geography</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Geology</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Paleontology</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Climatic changes</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Earth Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Geography</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Geology</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Paleontology</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield 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Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots.</subfield><subfield code="k">Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung</subfield><subfield code="y">z</subfield><subfield code="z">07-04-23</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">62</subfield><subfield code="1">01</subfield><subfield code="x">0028</subfield><subfield code="b">1315016974</subfield><subfield code="h">OLR-SEB</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. 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Contents … The Glacial and Loess Record of Southern South America … Introduction … The Glacial Record … Glaciations During the Latest Miocene, Early Pliocene and Middle Pliocene (Gilbert Chron) … Glaciations During the Late Pliocene (Gauss Chron) … Glaciations During the Early Pleistocene (Matuyama Chron) … The Great Patagonian Glaciation … Glaciations During the Middle-Late Pleistocene (Brunhes Chron) … The Late Pleistocene (Last Glacial Cycle: Brunhes Chron) … The Loess Record … Miocene-Pliocene Loess (Gauss-Gilbert Chron) … Pleistocene Loess (Brunhes-Matuyama-Gauss Chrons) … Last Glacial Cycle (Brunhes Chron) … References … The Glacial Record of Northern South America … Introduction … Glaciation During the Early Pleistocene (Matuyama Chron) … Glaciation During the Middle-Late Pleistocene (Brunhes Chron) … The Late Pleistocene (Last Glacial Cycle: Brunhes Chron) … References … The Glacial and Loess Record of North America … Introduction … Mountain and Continental Glaciation … Glaciations During the Late Pliocene: Pleistocene (Gilbert and Gauss/Matuyama, and Matuyama Chrons) … Glaciations During the Middle Pleistocene (Brunhes Chron) … VII viii Contents Glaciation During the Late Pleistocene (Brunhes Chron) … The Loess Record … References … Comparison of South and North American Glaciations … Glaciations During the Miocene-Pliocene (Gilbert and Gauss Chrons) and Early Pleistocene (Matuyama Chron) … Glaciations During the Middle and Late Pleistocene(Brunhes Chron) … References … Chinese Loess/Paleosol Record … References … Discussion and Conclusions … |
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Acknowledgments; Contents; Abstract; Introduction and Previous Work; 1 The Glacial and Loess Record of Southern South America; Abstract; Introduction; The Glacial Record; Glaciations During the Latest Miocene, Early Pliocene and Middle Pliocene (Gilbert Chron); Glaciations During the Late Pliocene (Gauss Chron); Glaciations During the Early Pleistocene (Matuyama Chron); The Great Patagonian Glaciation; Glaciations During the Middle-Late Pleistocene (Brunhes Chron)</subfield></datafield><datafield tag="505" ind1="8" ind2="0"><subfield code="a">The Late Pleistocene (Last Glacial Cycle: Brunhes Chron)The Loess Record; Miocene-Pliocene Loess (Gauss-Gilbert Chron); Pleistocene Loess (Brunhes-Matuyama-Gauss Chrons); Last Glacial Cycle (Brunhes Chron); References; 2 The Glacial Record of Northern South America; Abstract; Introduction; Glaciation During the Early Pleistocene (Matuyama Chron); Glaciation During the Middle-Late Pleistocene (Brunhes Chron); The Late Pleistocene (Last Glacial Cycle: Brunhes Chron); References; 3 The Glacial and Loess Record of North America; Abstract; Introduction; Mountain and Continental Glaciation</subfield></datafield><datafield tag="505" ind1="8" ind2="0"><subfield code="a">Glaciations During the Late Pliocene: Pleistocene (Gilbert and Gauss/Matuyama, and Matuyama Chrons)Glaciations During the Middle Pleistocene (Brunhes Chron); Glaciation During the Late Pleistocene (Brunhes Chron); The Loess Record; References; 4 Comparison of South and North American Glaciations; Abstract; Glaciations During the Miocene-Pliocene (Gilbert and Gauss Chrons) and Early Pleistocene (Matuyama Chron); Glaciations During the Middle and Late Pleistocene (Brunhes Chron); References; 5 Chinese Loess/Paleosol Record; Abstract; References; Discussion and Conclusions; References;</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Annotation, Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. 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Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="y">z</subfield><subfield code="z">29-07-12</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">65</subfield><subfield code="1">01</subfield><subfield code="x">0003</subfield><subfield code="b">1655668455</subfield><subfield code="c">03</subfield><subfield code="f">--%%--</subfield><subfield code="d">ebook</subfield><subfield code="e">--%%--</subfield><subfield code="j">--%%--</subfield><subfield code="h">OLR-SEB-ZDB-2-EES</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="y">k3o</subfield><subfield code="z">02-01-17</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">110</subfield><subfield code="1">01</subfield><subfield code="x">3110</subfield><subfield code="b">430502781X</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">s</subfield><subfield code="j">--%%--</subfield><subfield code="h">OLR-SEB</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots.</subfield><subfield code="y">z</subfield><subfield code="z">07-04-23</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">01</subfield><subfield code="x">0715</subfield><subfield code="b">1371379386</subfield><subfield code="h">OLR-ESP</subfield><subfield code="k">Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden.</subfield><subfield code="y">z</subfield><subfield code="z">15-03-13</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">02</subfield><subfield code="x">0715</subfield><subfield code="b">3577176105</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">g</subfield><subfield code="j">--%%--</subfield><subfield code="h">alma</subfield><subfield code="k">ww</subfield><subfield code="y">z</subfield><subfield code="z">20-01-20</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">03</subfield><subfield code="x">0715</subfield><subfield code="b">1752703995</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">g</subfield><subfield code="j">--%%--</subfield><subfield code="h">alma</subfield><subfield code="k">ww</subfield><subfield code="y">z</subfield><subfield code="z">22-02-18</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">285</subfield><subfield code="1">01</subfield><subfield code="x">0517</subfield><subfield code="b">1449601979</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">s</subfield><subfield code="j">--%%--</subfield><subfield code="h">OLR-ESP-EES</subfield><subfield code="k">Vervielfältigungen (z.B. 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