Cl concentrations in the Sajama ice core, and to a number of other pedological and geomorphological features indicative of long-term dry climates (8, 11–14, 18). This decline in human activity around the Altiplano paleolakes is seen in most caves, with early and late occupations separated by largely...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.125.8926 http://www.brc.dcs.gla.ac.uk/~drg/courses/sysbiomres/papers/Milo.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.125.8926 |
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openpolar |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.125.8926 2023-05-15T16:38:57+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.125.8926 http://www.brc.dcs.gla.ac.uk/~drg/courses/sysbiomres/papers/Milo.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.125.8926 http://www.brc.dcs.gla.ac.uk/~drg/courses/sysbiomres/papers/Milo.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.brc.dcs.gla.ac.uk/~drg/courses/sysbiomres/papers/Milo.pdf text ftciteseerx 2016-01-07T14:18:44Z Cl concentrations in the Sajama ice core, and to a number of other pedological and geomorphological features indicative of long-term dry climates (8, 11–14, 18). This decline in human activity around the Altiplano paleolakes is seen in most caves, with early and late occupations separated by largely sterile mid-Holocene sediments. However, a few sites, including the caves of Tulan-67 and Tulan-68, show that people did not completely disappear from the area. All of the sites of sporadic occupation are located near wetlands in valleys, near large springs, or where lakes turned into wetlands and subsistence resources were locally still available despite a generally arid climate Text ice core Unknown The Altiplano ENVELOPE(163.917,163.917,-78.133,-78.133) |
| institution |
Open Polar |
| collection |
Unknown |
| op_collection_id |
ftciteseerx |
| language |
English |
| description |
Cl concentrations in the Sajama ice core, and to a number of other pedological and geomorphological features indicative of long-term dry climates (8, 11–14, 18). This decline in human activity around the Altiplano paleolakes is seen in most caves, with early and late occupations separated by largely sterile mid-Holocene sediments. However, a few sites, including the caves of Tulan-67 and Tulan-68, show that people did not completely disappear from the area. All of the sites of sporadic occupation are located near wetlands in valleys, near large springs, or where lakes turned into wetlands and subsistence resources were locally still available despite a generally arid climate |
| author2 |
The Pennsylvania State University CiteSeerX Archives |
| format |
Text |
| url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.125.8926 http://www.brc.dcs.gla.ac.uk/~drg/courses/sysbiomres/papers/Milo.pdf |
| long_lat |
ENVELOPE(163.917,163.917,-78.133,-78.133) |
| geographic |
The Altiplano |
| geographic_facet |
The Altiplano |
| genre |
ice core |
| genre_facet |
ice core |
| op_source |
http://www.brc.dcs.gla.ac.uk/~drg/courses/sysbiomres/papers/Milo.pdf |
| op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.125.8926 http://www.brc.dcs.gla.ac.uk/~drg/courses/sysbiomres/papers/Milo.pdf |
| op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766029310801477632 |