Relationships between the stable isotopic signatures of living and fossil foraminifera in Monterey Bay, California

Abstract

Fossil foraminifera are critical to paleoceanographic reconstructions including estimates of past episodes of methane venting. These reconstructions rely on benthic foraminifera incorporating and retaining unaltered the ambient isotopic compositions of pore fluids and bottom waters. Comparisons are made here of isotopic compositions of abundant live and fossil foraminifera ( Uvigerina peregrina, Epistominella pacifica, Bulimina mexicana , and Globobulimina pacifica ) collected in Monterey Bay, CA from two cold seeps (Clam Flats and Extrovert Cliffs) and from sediments ∼5 m outside of the Clam Flats seep. Clam Flats has steep δ 13 C DIC gradients (to <−45‰), but DIC at Extrovert Cliffs is less enriched in 12 C (to approximately −22‰). Oxygen isotope values of fossil foraminifera at Clam Flats are ∼1.5‰ enriched in 18 O over the living foraminifera, as well as those of both live and fossil foraminifera at Extrovert Cliffs, suggesting they may have lived during the last glacial maximum. Statistical comparisons (Student's t and Kolmogorov‐Smirnov tests) of δ 13 C and δ 18 O values indicate that live and fossil foraminifera come from different populations at both Clam Flats and Extrovert Cliffs. At Clam Flats, the difference appears to result from alteration enriching some fossil foraminifera in 12 C over live foraminifera. At Extrovert Cliffs, the fossil foraminifera are enriched in 13 C over the live foraminifera, suggesting they lived prior to the onset of venting and thus that venting began recently. The short time of venting at Extrovert Cliffs may be responsible for the less alteration there compared with Clam Flats. These results indicate that preservation of foraminifera is likely to be poor within long‐lived cold seeps, but that foraminifera living in the surrounding sediment may incorporate and preserve broad basin‐wide changes in isotopic compositions of the ambient water.