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Biogenic carbonates in Antarctic marine sequences are critical to constrain reliable chronologies for Late Quaternary glacial/interglacial events. Increased amounts of iceberg rafted debris (IBRD) in ice-proximal sediments are proxies for climate-ind
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::156fe16c995b7e14507b4006bfcff9bc
http://hdl.handle.net/11368/1717245
http://hdl.handle.net/11368/1717245
