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PALEOCEANOGRAPHY

Southern Ocean Carbon and Nitrogen Isotopic Ratios

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Crosta, X., and A. Shemesh. 2002. Reconciling down-core anti-correlation of diatom carbon and nitrogen isotopic ratios from the Southern Ocean. Paleoceanography 17(1):1010.
Data Coverage North: -52.33 * South: -56.67
West: 20.78 * East: 160.23
Altitude: -3912 m

Data:     Please Cite Data Contributors!
  crosta2002
  io127010-tab.txt
  so136111-tab.txt

Summary:

Oceanic nutrient cycling in the Southern Ocean is supposed to have an important impact on glacial-interglacial atmospheric CO2 changes and global climate. In order to characterize such nutrient cycling over the last two climatic cycles, we investigated carbon and nitrogen isotopic ratios of diatom-bound organic matter (d13Cdiat and d15Ndiat respectively) in two cores retrieved form the Atlantic and Indian sectors of the Antarctic Ocean. The two cores show the same isotopic patterns. d13Cdiat values are depleted during glacial periods and enriched during interglacial periods indicating lower productivity during cold times. d15Ndiat values are enriched during glacial periods and depleted during interglacial periods arguing for greater nitrate utilization during cold times. Taken at face value, this apparent contradiction leads to opposite conclusions on the role of the Southern Ocean biological pump on the atmospheric CO2 changes. But, the two sets of data can be reconciled by a "sea ice + mixing rate scenario" that calls upon a balance between the effect of cutting off gas transfer at the ocean-atmosphere boundary and the effect of reducing vertical transport of nutrients through the pycnocline.
More Info on Paleoceanography Data

Parameters:

delta C13 PDB (diatom-bound organic matter); delta 15N (diatom-bound organic matter)

Complete XML Record:

noaa-ocean-2559  (Last Revised: 2007-12-21 )

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