Epibenthic foraminiferal δ¹³C in the Recent deep Arctic Ocean, supplement to: Mackensen, Andreas (2013): High epibenthic foraminiferal d13C in the recent deep Arctic Ocean: implications for ventilation and brine release during stadials. Paleoceanography, 28(3), 574-584

• Main Author: Mackensen, Andreas
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2013
• Subjects: Campaign of event; Event label; Date/Time of event; Latitude of event; Longitude of event; Elevation of event; DEPTH, sediment/rock; Cibicidoides spp., δ13C; Box corer; MultiCorer; Remote operated vehicle; Gravity corer; Giant box corer; MiniCorer; Multiple opening/closing net; Mass spectrometer Finnigan MAT 251 and Finnigan MAT 253; AOS94; ARA1B; ARA2B; ARA3B; HMMV; HE153; ARK-XIX/1; ARK-XIX/3c; ARK-XX/1; ARK-XX/3; ARK-XXIII/3; ARK-V/1; ARK-V/2; ARK-V/3b; ARK-VI/2; ARK-VII/3b; ARK-VIII/2; ARK-VIII/3; ARK-IX/3; ARK-IX/4; ARK-X/2; ARK-XI/1; ARK-XIII/2; ARK-XIII/3; Louis S. St-Laurent; Araon; L Atalante; Heincke; Polarstern; Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo; Andreas; Arctic; Arctic Ocean; Mendeleyev; Mendeleyev Ridge; Foraminifera*; Nordic Seas; Sea ice
• Online Access: https://dx.doi.org/10.1594/pangaea.819226; https://doi.pangaea.de/10.1594/PANGAEA.819226

Low planktic and benthic d18O and d13C values in sediments from the Nordic seas of cold stadials of the last glaciation have been attributed to brines, formed similar to modern ones in the Arctic Ocean. To expand on the carbon isotopes of this hypothesis I investigated benthic d13C from the modern A...