Environmental and Climatic Change as Recorded in Geological Sediments from the Arid to Semi-Arid Zone of China
| dc.contributor.author | Zhou, Weijian | |
| dc.contributor.author | Zhengkun, Wu | |
| dc.contributor.author | Jull, A. J. T. | |
| dc.contributor.author | Burr, G. | |
| dc.contributor.author | Donahue, D. D. | |
| dc.contributor.author | Baosheng, Li | |
| dc.contributor.author | Head, J. | |
| dc.date.accessioned | 2021-02-11T21:32:17Z | |
| dc.date.available | 2021-02-11T21:32:17Z | |
| dc.date.issued | 2001-01-01 | |
| dc.identifier.citation | Zhou, W., Zhengkun, W., Jull, A. J. T., Burr, G., Donahue, D. D., Baosheng, L., & Head, J. (2001). Environmental and climatic change as recorded in geological sediments from the arid to semi-arid zone of China. Radiocarbon, 43(2B), 619-627. | |
| dc.identifier.issn | 0033-8222 | |
| dc.identifier.doi | 10.1017/S0033822200041278 | |
| dc.identifier.uri | http://hdl.handle.net/10150/654498 | |
| dc.description | From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000. | |
| dc.description.abstract | Stratigraphic investigations together with climatic proxy data measurements and reliable radiocarbon dating show a history of fluctuations of dry and wet environmental conditions in the arid to semi-arid zone of northern China since the late Pleistocene. Based on these data, we are able to reconstruct shifts of the desert margin in two period extremes, the last glacial maximum (21-15 ka) and the Holocene Optimum (9-5 ka). We have compared the present desert margin with that for the two extremes. The results indicate that a southward shift of the present margin of about 3 degrees in latitude might be caused by anthropogenic impact. Hence the influence of human activity must be taken into consideration for sustainable development and environment protection. Future research will be to find a two-way feedback existing between climate and anthropogenic impacts. | |
| dc.language.iso | en | |
| dc.publisher | Department of Geosciences, The University of Arizona | |
| dc.relation.url | http://radiocarbon.webhost.uits.arizona.edu/ | |
| dc.rights | Copyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved. | |
| dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | |
| dc.subject | protection | |
| dc.subject | sustainable development | |
| dc.subject | arid environment | |
| dc.subject | lithostratigraphy | |
| dc.subject | China | |
| dc.subject | fluctuations | |
| dc.subject | climate change | |
| dc.subject | semi arid environment | |
| dc.subject | terrestrial environment | |
| dc.subject | human activity | |
| dc.subject | Holocene | |
| dc.subject | Far East | |
| dc.subject | paleoclimatology | |
| dc.subject | Pleistocene | |
| dc.subject | upper Pleistocene | |
| dc.subject | sediments | |
| dc.subject | Asia | |
| dc.subject | Cenozoic | |
| dc.subject | Quaternary | |
| dc.subject | C 14 | |
| dc.subject | carbon | |
| dc.subject | dates | |
| dc.subject | isotopes | |
| dc.subject | radioactive isotopes | |
| dc.subject | absolute age | |
| dc.title | Environmental and Climatic Change as Recorded in Geological Sediments from the Arid to Semi-Arid Zone of China | |
| dc.type | Proceedings | |
| dc.type | text | |
| dc.identifier.journal | Radiocarbon | |
| dc.description.collectioninformation | The Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information. | |
| dc.eprint.version | Final published version | |
| dc.description.admin-note | Migrated from OJS platform February 2021 | |
| dc.source.volume | 43 | |
| dc.source.issue | 2B | |
| dc.source.beginpage | 619 | |
| dc.source.endpage | 627 | |
| refterms.dateFOA | 2021-02-11T21:32:17Z |
