Oxygen isotope (δ¹⁸O) values of benthic ostracods from varved sediments from Mondsee (Austria) for the interval 7.7-8.7 ka BP, supplement to: Andersen, Nils; Lauterbach, Stefan; Erlenkeuser, Helmut; Danielopol, Dan L; Namiotko, Tadeusz; Hüls, Matthias; Belmecheri, Soumaya; Dulski, Peter; Nantke, Carla; Meyer, Hanno; Chapligin, Bernhard; von Grafenstein, Ulrich; Brauer, Achim (2017): Evidence for higher-than-average air temperatures after the 8.2 ka event provided by a Central European d18O record. Quaternary Science Reviews, 172, 96-108

• Main Authors: Andersen, Nils, Lauterbach, Stefan, Erlenkeuser, Helmut, Danielopol, Dan L, Namiotko, Tadeusz, Hüls, Matthias, Belmecheri, Soumaya, Dulski, Peter, Nantke, Carla, Meyer, Hanno, Chapligin, Bernhard, von Grafenstein, Ulrich, Brauer, Achim
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2017
• Subjects: DEPTH, sediment/rock; Varve age; AGE; Ostracoda, δ18O; δ18O, water; Piston corer, UWITEC; Reconstructed; Hanno; Nils; North Atlantic
• Online Access: https://dx.doi.org/10.1594/pangaea.880316; https://doi.pangaea.de/10.1594/PANGAEA.880316

The so-called 8.2 ka event represents one of the most prominent cold climate anomalies during the Holocene warm period. Accordingly, several studies have addressed its trigger mechanisms, absolute dating and regional characteristics so far. However, knowledge about subsequent climate recovery is sti...