Underlying causes for long-term global ocean δ13C fluctuations over the last 1.20 Myr

Details Underlying causes for long-term global ocean δ13C fluctuations over the last 1.20 Myr Underlying causes for long-term global ocean δ13C fluctuations over the last 1.20 Myr

Aug 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006e%26psl.248...15h&link_type=abstract

Earth and Planetary Science Letters, Volume 248, Issue 1-2, p. 15-29.

Physics

11

Scientific paper

Pleistocene stable carbon isotope (δ13C) records from surface and deep dwelling foraminifera in all major ocean basins show two distinct long-term carbon isotope fluctuations since 1.00 Ma. The first started around 1.00 Ma and was characterised by a 0.35‰ decrease in δ13C values until 0.90 Ma, followed by an increase of 0.60‰ lasting until 0.50 Ma. The subsequent fluctuation started with a 0.40‰ decrease between 0.50 and 0.25 Ma, followed by an increase of 0.30‰ between 0.25 and 0.10 Ma. Here, we evaluate existing evidence and various hypotheses for these global Pleistocene δ13C fluctuations and present an interpretation, where the fluctuations most likely resulted from concomitant changes in the burial fluxes of organic and inorganic carbon due to ventilation changes and/or changes in the production and export ratio. Our model indicates that to satisfy the long-term ‘stability’ of the Pleistocene lysocline, the ratio between the amounts of change in the organic and inorganic carbon burial fluxes would have to be close to a 1:1 ratio, as deviations from this ratio would lead to sizable variations in the depth of the lysocline. It is then apparent that the mid-Pleistocene climate transition, which, apart from the glacial cycles, represents the most fundamental change in the Pleistocene climate, was likely not associated with a fundamental change in atmospheric pCO2. While recognising that high frequency glacial/interglacial cycles are associated with relatively large (100 ppmv) changes in pCO2, our model scenario (with burial changes close to a 1:1 ratio) produces a maximum long-term variability of only 20 ppmv over the fluctuation between 1.00 and 0.50 Ma.

Affiliated with

Also associated with

No associations

Rating

Underlying causes for long-term global ocean δ13C fluctuations over the last 1.20 Myr does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Underlying causes for long-term global ocean δ13C fluctuations over the last 1.20 Myr, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Underlying causes for long-term global ocean δ13C fluctuations over the last 1.20 Myr will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-975698