Arid
DOI10.1016/S0921-8181(00)00063-1
A 22,000 C-14 year BP sediment and pollen record of climate change from Laguna Miscanti (23 degrees S), northern Chile
Grosjean, M; van Leeuwen, JFN; van der Knaap, WO; Geyh, MA; Ammann, B; Tanner, W; Messerli, B; Nunez, LA; Valero-Garces, BL; Veit, H
通讯作者Grosjean, M
来源期刊GLOBAL AND PLANETARY CHANGE
ISSN0921-8181
出版年2001
卷号28期号:1-4页码:35-51
英文摘要

Lake sediments and pollen, spores and algae from the high-elevation endorheic Laguna Miscanti (22 degrees 45’s, 67 degrees 45’W, 4140 m a.s.l., 13.5 km(2) water surface, 10 m deep) in the Atacama Desert of northern Chile provide information about abrupt and high amplitude changes in effective moisture. Although the lack of terrestrial organic macrofossils and the presence of a significant C-14 reservoir effect make radiocarbon dating of lake sediments very difficult, we propose the following palaeoenvironmental history. An initial shallow freshwater lake (ca. 22,000 C-14 years BP) disappeared during the extremely dry conditions of the Last Glacial Maximum (LGM; 18,000 C-14 years BP). That section is devoid of pollen. The late-glacial lake transgression started around 12,000 C-14 years BP, peaked in two phases between ca. 11,000 and < 9000 C-14 years BP, and terminated around 8000 C-14 years BP. Effective moisture increased more than three times compared to modern conditions ( 200 mm precipitation), and a relatively dense terrestrial vegetation was established. Very shallow hypersaline lacustrine conditions prevailed during the mid-Holocene until ca. 3600 C-14 years BP, However, numerous drying and wetting cycles suggest frequent changes in moisture, maybe even individual storms during the mid-Holocene. After several humid spells, modern conditions were reached at ca. 3000 C-14 years BP, Comparison between limnogeological data and pollen of terrestrial plants suggest century-scale response lags. Relatively constant concentrations of long-disance transported pollen from lowlands east of the Andes suggest similar atmospheric circulation patterns (mainly tropical summer rainfall) throughout the entire period of time. These findings compare favorably with other regional paleoenvironmental data. (C) 2001 Elsevier Science B.V. All rights reserved.


英文关键词Holocene Pleistocene lake sediments pollen radiocarbon reservoir effect Andes
类型Article
语种英语
国家Switzerland ; Germany ; Chile ; Spain
收录类别SCI-E
WOS记录号WOS:000167607300006
WOS关键词LAKE-TITICACA ; ATACAMA-ALTIPLANO ; BOLIVIAN ALTIPLANO ; TROPICAL ANDES ; EARLY HOLOCENE ; PALEOHYDROLOGY ; LIMNOGEOLOGY ; LACUSTRINE ; PERU
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/140829
作者单位(1)Univ Bern, Dept Phys Geog, CH-3012 Bern, Switzerland;(2)Univ Bern, Geobot Inst, CH-3013 Bern, Switzerland;(3)German Geol Survey, Joint Geosci Res Inst, D-30631 Hannover, Germany;(4)Univ Catolica Norte, Inst Invest Arqueol, San Pedro, Atacama, Chile;(5)CSIC, Inst Pirenaico Ecol, E-50080 Zaragoza, Spain
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GB/T 7714
Grosjean, M,van Leeuwen, JFN,van der Knaap, WO,et al. A 22,000 C-14 year BP sediment and pollen record of climate change from Laguna Miscanti (23 degrees S), northern Chile[J],2001,28(1-4):35-51.
APA Grosjean, M.,van Leeuwen, JFN.,van der Knaap, WO.,Geyh, MA.,Ammann, B.,...&Veit, H.(2001).A 22,000 C-14 year BP sediment and pollen record of climate change from Laguna Miscanti (23 degrees S), northern Chile.GLOBAL AND PLANETARY CHANGE,28(1-4),35-51.
MLA Grosjean, M,et al."A 22,000 C-14 year BP sediment and pollen record of climate change from Laguna Miscanti (23 degrees S), northern Chile".GLOBAL AND PLANETARY CHANGE 28.1-4(2001):35-51.
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