Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Middle to Late Holocene Fluctuations of C3 and C4 Vegetation in a Northern New England Salt Marsh, Sprague Marsh, Phippsburg Maine

Journal Article · · Organic Geochemistry
OSTI ID:902243

A 3.1 meter sediment core was analyzed for stable carbon isotope composition of organic matter and higher plant leaf wax (HPLW) lipid biomarkers to determine Holocene shifts in C{sub 3} (higher high marsh) and C{sub 4} (low and/or high marsh) plant deposition at the Sprague River Salt Marsh, Phippsburg, Maine. The carbon isotope composition of the bulk sediment and the HPLW parallel each other throughout most of the core, suggesting that terrestrial plants are an important source of organic matter to the sediments, and diagenetic alteration of the bulk sediments is minimal. The current salt marsh began to form 2500 cal yr BP. Low and/or high C{sub 4} marsh plants dominated deposition at 2000 cal yr BP, 700 cal yr BP, and for the last 200 cal yr BP. Expansion of higher high marsh C{sub 3} plants occurred at 1300 and 600 cal yr BP. These major vegetation shifts result from a combination of changes in relative sea-level rise and sediment accumulation rates. Average annual carbon sequestration rates for the last 2500 years approximate 40 g C yr{sup -1} m{sup -2}, and are in strong agreement with other values published for the Gulf of Maine. Given that Maine salt marshes cover an area of {approx}79 km{sup 2}, they represent an important component of the terrestrial carbon sink. More detailed isotopic and age records from a network of sediment cores at Sprague Marsh are needed to truly evaluate the long term changes in salt marsh plant communities and the impact of more recent human activity, including global warming, on salt marsh vegetation.

Research Organization:
Lawrence Livermore National Laboratory (LLNL), Livermore, CA
Sponsoring Organization:
USDOE
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
902243
Report Number(s):
UCRL-JRNL-221751
Journal Information:
Organic Geochemistry, Journal Name: Organic Geochemistry Journal Issue: 3 Vol. 38; ISSN 0146-6380; ISSN ORGEDE
Country of Publication:
United States
Language:
English

Similar Records

Stable isotopes, Sr/Ca, and Mg/Ca in biogenic carbonates from Petaluma Marsh, northern California, USA
Journal Article · Thu Oct 01 00:00:00 EDT 1998 · Geochimica et Cosmochimica Acta · OSTI ID:338611

Stable isotopes, Sr/Ca, and Mg/Ca in biogenic carbonates from Petaluma Marsh, northern California, USA
Journal Article · Tue Oct 19 00:00:00 EDT 2004 · Geochimica et Cosmochimica Acta · OSTI ID:833680

Differentiating climatic and successional influences on long-term development of a marsh
Journal Article · Sun Sep 01 00:00:00 EDT 1996 · Ecology · OSTI ID:513387