The use of δ13C signature of C-3 and C-4 plants in determining past depositional environments in rapidly accreting marshes of the Mississippi River deltaic plain, Louisiana, U.S.A.-Reference-Cited by-同舟云学术

The use of δ13C signature of C-3 and C-4 plants in determining past depositional environments in rapidly accreting marshes of the Mississippi River deltaic plain, Louisiana, U.S.A.

Published:1986-01 Issue: Volume:59 Page:315-320
ISSN:0168-9622
Container-title:Chemical Geology: Isotope Geoscience section
language:en
Short-container-title:Chemical Geology: Isotope Geoscience section

Author:

DeLaune R.D

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference16 articles.

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3. Carbon isotope distribution in the Pamlico River Estuary, North Carolina and tributaries;Brinson;Estuaries,1983

4. Sedimentation rates determined by 137Cs dating in a rapidly accreting salt marsh;DeLaune;Nature (London),1978

5. Fresh water peat on the continental shelf;Emery;Science,1967

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