Carbon isotope (d13C) excursions suggest times of major methane release during the last 14 ka in Fram Strait, the deep-water gateway to the Arctic

dc.contributor.author	Consolaro, Chiara
dc.contributor.author	Rasmussen, Tine Lander
dc.contributor.author	Panieri, Giuliana
dc.contributor.author	Mienert, Jurgen
dc.contributor.author	Bünz, Stefan
dc.contributor.author	Sztybor, Kamila
dc.date.accessioned	2015-03-16T08:48:53Z
dc.date.available	2015-03-16T08:48:53Z
dc.date.issued	2014
dc.identifier.citation	Climate of the Past Discussions 10(2014) s. 4191-4227	en_US
dc.identifier.cristinID	FRIDAID 1199990
dc.identifier.doi	10.5194/cpd-10-4191-2014
dc.identifier.issn	1814-9340
dc.identifier.uri	https://hdl.handle.net/10037/7510
dc.identifier.urn	URN:NBN:no-uit_munin_7103
dc.language.iso	eng	en_US
dc.publisher	European Geosciences Union	en_US
dc.rights.accessRights	openAccess
dc.subject	VDP:466	en_US
dc.subject	VDP::464	en_US
dc.title	Carbon isotope (d13C) excursions suggest times of major methane release during the last 14 ka in Fram Strait, the deep-water gateway to the Arctic	en_US
dc.type	Journal article	en_US
dc.type	Tidsskriftartikkel	en_US
dc.type	Peer reviewed	en_US