Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific

Authors

Rebecca S. Robinson, University of Rhode Island
P. Martinez
L. D. Pena
I. Cacho

Document Type

Article

Date of Original Version

2009

Department

Oceanography

Abstract

The Eastern Equatorial Pacific (EEP) is a high nutrient–low chlorophyll region of the ocean. Downcore nitrogen isotope records from the EEP have been previously interpreted as a direct reflection of changes in nutrient consumption. However, the observed changes in sedimentary δ¹⁵N since the last glacial maximum have no coherent relationship with export productivity or an inferred variation in the iron‐to‐nitrate ratio of the surface waters. Rather, downcore N isotope records in the EEP strongly resemble changes in the extent of water column denitrification as recorded in nearby sedimentary δ¹⁵N records along the western margin of the Americas. This similarity is attributed to the overprinting of the N isotopic composition of nitrate in the EEP through the advection of nitrate westward from the margins in the subsurface. A local nitrogen isotope record of changes in the degree of nutrient consumption is extracted from the bulk sedimentary record by subtracting two different sedimentary δ¹⁵N records of denitrification changes from two new EEP δ¹⁵N records (TR163‐22 and ODP Site 1240). The denitrification records used are from 1) the Central American margin (ODP Site 1242) and 2) the South American margin (GeoB7139‐2). The degree of consumption in the surface waters declines rapidly from elevated values during the last glacial maximum to a pair of minima around 15 and 11–13 ka, and finally it increases into the Holocene. The derived EEP nitrogen isotope record indicates that the regional peak in export productivity occurred when the supply of nutrients exceeded the apparently high demand. The influx of nutrients during the deglaciation is attributed to the resumption of intense overturning in the Southern Ocean and the release of sequestered CO₂ and nutrient‐rich, O₂ poor waters from the deep ocean. This has important implications for understanding the glacial‐interglacial scale variation in intermediate water suboxia and water column denitrification.

Citation/Publisher Attribution

Robinson, R. S., P. Martinez, L. D. Pena, and I. Cacho (2009), Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific, Paleoceanography, 24, PA4213, doi: 10.1029/2008PA001702.

Available at: https://doi.org/10.1029/2008PA001702