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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| Main Authors: | , , , , |
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| Format: | Article |
| Language: | en |
| Published: |
AGU and Geochemical Society
2013
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| 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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