In:
Boreas, Wiley, Vol. 41, No. 4 ( 2012-10), p. 707-718
Abstract:
We present elemental concentrations and magnetic susceptibility data from a new 270‐cm‐long sediment core collected from the western part of palaeolake B abicora and infer millennial‐scale hydrological variations over the last 27 cal. ka in the western C hihuahua D esert. Variations in the available water content at the sediment–air interface of the watershed, lake salinity and lake productivity are inferred from values of the chemical index of alteration ( CIA ), CaCO 3 and C org , respectively. An abrupt increase in runoff at c . 24 cal. ka BP appears correlative with the H einrich 2 ( H 2) event. Except for this event, diminished runoff between c . 27 and 19 cal. ka BP indicates lower annual precipitation (weak summer rainfall) during the Last Glacial Maximum. The deposition of chemically altered sediments between c . 25 and 22 cal. ka BP results from the higher sediment–water interaction in the watershed owing to lower evaporation, cooler conditions and higher precipitation during the H2 event. Since 19 cal. ka BP the runoff has been characterized by high‐amplitude fluctuations with intervals of reduced precipitation identified at c . 19, 18, 17.5, 13–14, 11.5, 10, 7.5 and 3 cal. ka BP .
Type of Medium:
Online Resource
ISSN:
0300-9483
,
1502-3885
DOI:
10.1111/bor.2012.41.issue-4
DOI:
10.1111/j.1502-3885.2012.00266.x
Language:
English
Publisher:
Wiley
Publication Date:
2012
detail.hit.zdb_id:
2028632-6
detail.hit.zdb_id:
185110-X
SSG:
14
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