American Geophysical Union Become an AGU Member
Subscribe to AGU Journals		 AGU Home AGU Publications

Read Full Article (file size: 555341 bytes)    Cited by

PALEOCEANOGRAPHY, VOL. 19, PA4010, doi:10.1029/2004PA001026, 2004

Ground-truthing the boron isotope-paleo-pH proxy in planktonic foraminifera shells: Partial dissolution and shell size effects

Bärbel Hönisch

School of Earth and Environmental Sciences, Queens College, Flushing, New York, USA


N. Gary Hemming

School of Earth and Environmental Sciences, Queens College, Flushing, New York, USA


Abstract

Sediment samples from the Ontong-Java Plateau in the Pacific and the 90° east ridge in the Indian Ocean were used to investigate whether shell size and early diagenesis affect δ11B of the symbiont-bearing planktonic foraminifer Globigerinoides sacculifer. In pristine shells from both study locations we found a systematic increase of δ11B and Mg/Ca with shell size. Shells in the sieve size class 515–865 μm revealed δ11B values +2.1 to +2.3‰ higher than shells in the 250–380 μm class. This pattern is most likely due to differences in symbiont photosynthetic activity and its integrated effect on the pH of the foraminiferal microenvironment. We therefore suggest smaller individuals must live at approximately 50–100 m water depth where ambient light levels are lower. Using the empirical calibration curve for δ11B in G. sacculifer, only shells larger than 425 μm reflect surface seawater pH. Partial dissolution of shells derived from deeper sediment cores was determined by shell weight analyses and investigation of the shell surface microstructure by scanning electron microscopy. The δ11B in partially dissolved shells is up to 2‰ lower relative to pristine shells of the same size class. In agreement with a relatively higher weight loss in smaller shells, samples from the Ontong-Java Plateau show a more pronounced dissolution effect than larger shells. On the basis of the primary size effect and potential postdepositional dissolution effects, we recommend the use of shells that are visually pristine and, in the case of G. sacculifer, larger than 500 μm for paleoreconstructions.

Received 5 March 2004; accepted 25 August 2004; published 3 November 2004.

Keywords: dissolution; shell size; δ11B.

Index Terms: 1050 Geochemistry: Marine geochemistry (4835, 4850); 4267 Oceanography: General: Paleoceanography; 4806 Oceanography: Biological and Chemical: Carbon cycling; 4870 Oceanography: Biological and Chemical: Stable isotopes; 4855 Oceanography: Biological and Chemical: Plankton.

Read Full Article (file size: 555341 bytes)    Cited by

Citation: Hönisch, B., and N. G. Hemming (2004), Ground-truthing the boron isotope-paleo-pH proxy in planktonic foraminifera shells: Partial dissolution and shell size effects, Paleoceanography, 19, PA4010, doi:10.1029/2004PA001026.