OC3 - Ocean Circulation and Carbon Cycling
Summary OC3 focusses on reconstructing ocean circulation and carbon cycling over the last 20,000 years by synthesizing carbon isotopes (d13C) measured on shells of benthic foraminifera from sediments of all ocean basins. More than 90 international scientists are involved.Sign up to the OC3 mailing list.Goals - To synthesize core-top data and compare to water-column measurements for a new global calibration (completed).
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Launch |
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Synthesis |
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2014 |
2015-17 |
2018 |
2019 |
Changes in the amount of carbon stored in the oceans are thought to have played an important role in past variations of atmospheric CO2 and climate. Deep circulation controls the ocean's storage and redistribution of heat and carbon. Climate changes in turn affect physical (e.g. dust and iron supply, mixing, upwelling) and biological (e.g. plankton productivity) processes in the oceans.
Recent model simulations imply that a combination of these processes could explain glacial-interglacial CO2 variations. New paleodata reveal the transition of circulation, atmospheric CO2, and climate from the Last Glacial Maximum (~21,000 years ago) to the present in unprecedented detail including several rapid changes; however, the evidence from the deep ocean is still extremely limited.
Extension 2019
Due to extensive labor that is needed to generate consistent age models as well as to ensure data quality, the group has been extended for one year to finish the work. During the first years of OC3, strategies for the data synthesis, data storage and age-model generation have been developed. Additional to the workshop reports, regional syntheses for the Southern Ocean sector of the Atlantic and Pacific, and a global coretop δ13C compilation, have been published (see Products).
The data collection is set up in close collaboration with NOAA (Carrie Morrill) and PANGAEA (in house MARUM) and will be made available through NOAA and PANGAEA.
Planned timeline for the extension
October 2018: Release of the final database structure
January 2019: Accomplishment of version 0 of database
February 2019: Submission of manuscript with the regional North Atlantic dataset
February 2019: Submission of manuscript describing OC3 database, release of database version 0 together with database paper
February to June 2019: Collection of unpublished datasets, compilation of global dataset
EGU 2019: Splinter meeting of joint IPODS and OC3 group
December 2019: AGU session with OC3 associated topic
Link to the external OC3 website.
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Observed δ13C distribution in the water column (top; Schmittner et al. 2013) and in surface (Late Holocene) sediments (second from top), in LGM sediments (third from top), and the LGM-LH difference (bottom) (Schmittner, PAGES News (2012), 20:1, 17) |
Learn more and participate
To subscribe to the OC3 mailing list or find out more about contributing to the group, click here.
Logo
Download the OC3 logo (png) (zip).
Past publications and presentations
> Report on Preliminary Database (Atlantic) by Emma Gleeman (Research Experience for Undergraduates Student Summer 2015)
> Report on Preliminary Database (Indian & Pacific) by Aaron Rachels (Research Experience for Undergraduates Student Summer 2015)
> Poster at AGU Fall Meeting 2015 - Global Calibration of Benthic Foranimiferal Carbon Isotope Ratios.
Meeting minutes
> November 2015
> September 2015