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

[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 f...

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Bibliographic Details
Main Authors: Judson W, Partin, Kim M, Cobb, Jess F, Adkins, Andrew Alek, Tuen, Brian, Clark
Format: Article
Language:English
Published: AGU and Geochemical Society 2013
Subjects:
Online Access:http://ir.unimas.my/id/eprint/7001/1/Judson%20W.pdf
http://ir.unimas.my/id/eprint/7001/
http://www.researchgate.net/publication/260249435_Trace_metal_and_carbon_isotopic_variations_in_cave_dripwater_and_stalagmite_geochemistry_from_northern_Borneo
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