Planktic foraminifera counts from sediment core Fr1/94-GC3, Tasman Sea (1994)

This core was obtained in January 1994 by the RV Franklin using a gravity corer at a depth of 2667 m at 44°15.38’ S, 149°59.47’E. It is 4.71 m long and is almost uniformly olive grey clay (5Y, 5/1–6/2). The coarse [>150 μm] fraction consists almost entirely of biogenic carbonates. The core was found to span the last 460 ka, representing four glacial–interglacial cycles. Data from PANGAEA (https://doi.pangaea.de/10.1594/PANGAEA.946026) accessed on 2022-11-01

Citation: De Deckker, Patrick; Barrows, Timothy T; Stuut, Jan-Berend W; van der Kaars, Sander; Ayress, M A; Rogers, John; Chaproniere, George C H (2022): Planktic foraminifera counts from sediment core Fr1/94-GC3. PANGAEA, (https://doi.pangaea.de/10.1594/PANGAEA.946026

Published: July 01, 2023 at 06:52

URL: https://www.marine.csiro.au/ipt/resource?r=fr199401_gc3_forams