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May 23, 2013 11:33 GMT
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Apr 24, 2013 4:41 GMT
Keck / AMS Lab
For more information, see http://www.ess.uci.edu/ams
Recent (<4 year old) leaf litter is not a major source of microbial carbon in a temperate forest mineral soil
(2010). Recent (<4 year old) leaf litter is not a major source of microbial carbon in a temperate forest mineral soil.
Soil Biology and Biochemistry. 42, 1028-1037.
Sources, composition, and fate of suspended particulate organic. Carbon of a small mountainous river
(2003). Sources, composition, and fate of suspended particulate organic. Carbon of a small mountainous river.
Abstracts of Papers American Chemical Society. 225, 117.
Sedimentary rocks as sources of ancient organic carbon to the ocean: An investigation through Delta C-14 and delta C-13 signatures of organic compound classes
(2005). Sedimentary rocks as sources of ancient organic carbon to the ocean: An investigation through Delta C-14 and delta C-13 signatures of organic compound classes.
Global Biogeochemical Cycles. 19,
Fossil methane source dominates Cariaco Basin water column methane geochemistry
(2005). Fossil methane source dominates Cariaco Basin water column methane geochemistry.
Geophysical Research Letters. 32,
Small-mass graphite preparation by sealed tube zinc reduction method for AMS (14)C measurements
(2010). Small-mass graphite preparation by sealed tube zinc reduction method for AMS (14)C measurements.
Nuclear Instruments & Methods in Physics Research Section B-Beam Interactions with Materials and Atoms. 268, 927-930.
Prehistoric human impacts on Rapa, French Polynesia
(2006). Prehistoric human impacts on Rapa, French Polynesia.
Antiquity. 80, 340-354.
Basin-wide estimates of the input of methane from seeps and clathrates to the Black Sea
(2006). Basin-wide estimates of the input of methane from seeps and clathrates to the Black Sea.
Earth and Planetary Science Letters. 243, 366-375.
Carbon isotope ratios of organic compound fractions in oceanic suspended particles
(2006). Carbon isotope ratios of organic compound fractions in oceanic suspended particles.
Geophysical Research Letters. 33,
Source(s) and cycling of the nonhydrolyzable organic fraction of oceanic particles
(2006). Source(s) and cycling of the nonhydrolyzable organic fraction of oceanic particles.
Geochimica Et Cosmochimica Acta. 70,
Incorporation of aged dissolved organic carbon (DOC) by oceanic particulate organic carbon (POC): An experimental approach using natural carbon isotopes
(2006). Incorporation of aged dissolved organic carbon (DOC) by oceanic particulate organic carbon (POC): An experimental approach using natural carbon isotopes.
Marine Chemistry. 98, 315-322.