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Results of the Q-mode principal component (PC) analysis
Funding: Response to environmental changes and post-industrial recovery of foraminifera from South Georgia fjords, sub-Antarctic (Award: 2018/31/B/ST10/02886) -
Benthic foraminifera (stained) in sub-Antarctic fjords of South Georgia
We present a baseline study of “living” (rose Bengal stained) benthic foraminifera from fjords of South Georgia, including fjords with and without tidewater glaciers. Their... -
Foraminiferal census data for the >63 µm fraction of diverse environments of ...
Funding: Response to environmental changes and post-industrial recovery of foraminifera from South Georgia fjords, sub-Antarctic (Award: 2018/31/B/ST10/02886) -
Foraminiferal census data for the >125 µm fraction of diverse environments of...
Funding: Response to environmental changes and post-industrial recovery of foraminifera from South Georgia fjords, sub-Antarctic (Award: 2018/31/B/ST10/02886) -
Foraminiferal census data for the 63-125 µm fraction of diverse environments ...
Funding: Response to environmental changes and post-industrial recovery of foraminifera from South Georgia fjords, sub-Antarctic (Award: 2018/31/B/ST10/02886) -
Environmental parameters and sediment properties discussed in this study and ...
Funding:Response to environmental changes and post-industrial recovery of foraminifera from South Georgia fjords, sub-Antarctic (Award: 2018/31/B/ST10/02886) -
Alkenone determination from sediment core TAN1106/28
Over the last deglaciation there were two transient intervals of pronounced atmospheric CO2 rise; Heinrich Stadial 1 (17.5-15 kyr) and the Younger Dryas (12.9-11.5 kyr). Leading... -
δ13C and δ18O isotopes of Globigerina bulloides from ODP Site 177-1090
Over the last deglaciation there were two transient intervals of pronounced atmospheric CO2 rise; Heinrich Stadial 1 (17.5-15 kyr) and the Younger Dryas (12.9-11.5 kyr). Leading... -
δ11B isotopes, CO2 release and pH analysis from sedeiment core TAN1106/28
Over the last deglaciation there were two transient intervals of pronounced atmospheric CO2 rise; Heinrich Stadial 1 (17.5-15 kyr) and the Younger Dryas (12.9-11.5 kyr). Leading... -
δ11B isotopes, CO2 release and pH analysis from ODP Site 177-1090
Over the last deglaciation there were two transient intervals of pronounced atmospheric CO2 rise; Heinrich Stadial 1 (17.5-15 kyr) and the Younger Dryas (12.9-11.5 kyr). Leading...