Organic and black carbon 13 C and 14 C through the Santa Monica Basin sediment oxic‐anoxic transition-Reference-Cited by-同舟云学术

Organic and black carbon 13 C and 14 C through the Santa Monica Basin sediment oxic‐anoxic transition

Published:2003-02 Issue:4 Volume:30 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Masiello C. A.¹²,Druffel E. R. M.¹

Affiliation:

1. Department of Earth System Science University of California at Irvine Irvine California USA

2. Now at Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, 7000 East Ave, P.O. Box 808, Livermore, CA, USA and Division of Geology and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA.

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2002GL015050

Reference28 articles.

1. Inter-decadal signals during the last millennium (AD 1117-1992) in the Varve record of Santa Barbara Basin, California

2. Non-annual laminations and expansion of anoxic basin-floor conditions in Santa Monica Basin, California Borderland, over the past four centuries

3. Cycling of dissolved and particulate organic matter in the open ocean

4. Natural and anthropogenic changes in atmospheric CO2over the last 1000 years from air in Antarctic ice and firn

5. Geochemical and sedimentologic variations in inter-annually laminated sediments from Santa Monica Basin

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