Trace metal and carbon isotopic variations in cave dripwater and stalagmite geochemistry from northern Borneo

Judson W, Partin and Kim M, Cobb and Jess F, Adkins and Andrew Alek, Tuen and Brian, Clark (2013) Trace metal and carbon isotopic variations in cave dripwater and stalagmite geochemistry from northern Borneo. Geochemistry, Geophysics, Geosystems, 14 (9). pp. 3567-3585. ISSN 1525-2027

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Official URL: http://www.researchgate.net/publication/260249435_...

Abstract

[2] Stalagmites are valuable archives of terrestrial paleoclimate because they form in karst systems located around the world, can be absolute-dated, and afford high-resolution reconstructions on glacialinterglacial timescales. Stalagmite oxygen isotopic composition (18O) is the primary proxy used for stalagmite paleoclimate reconstructions because it reflects changes in rainfall 18O that are related to rainfall amount [Dansgaard, 1964; Rozanski et al.

Item Type:	Article
Uncontrolled Keywords:	Major and trace element geochemistry , Geochemistry , Stable isotope geochemistry , Isotopic composition and chemistry , Biogeosciences , unimas, university, universiti, Borneo, samarahan, ipta, education, research, Universiti Malaysia Sarawak, Sarawak, kuching,
Subjects:	G Geography. Anthropology. Recreation > GE Environmental Sciences
Divisions:	Academic Faculties, Institutes and Centres > Institute of Biodiversity and Environmental Conservation Faculties, Institutes, Centres > Institute of Biodiversity and Environmental Conservation
Depositing User:	Karen Kornalius
Date Deposited:	21 Apr 2015 07:35
Last Modified:	25 Jan 2022 06:31
URI:	http://ir.unimas.my/id/eprint/7001

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