Sedimentary environments in the south-western Barents Sea during the last deglaciation and the Holocene: a case study outside the Ingøydjupet trough
A lithological and foraminiferal study of newly acquired sediment cores outside the Ingøydjupet (Ingøy Deep) trough has been carried out to improve constraints on the last deglacial history in the south-western Barents Sea. Three lithofacies and three foraminiferal facies were identified. The lowerm...
Main Authors: | Mauro Pau, Øyvind Hammer |
---|---|
Format: | Article |
Language: | English |
Published: |
Norwegian Polar Institute
2016-05-01
|
Series: | Polar Research |
Subjects: | |
Online Access: | http://www.polarresearch.net/index.php/polar/article/view/23104/pdf_78 |
Similar Items
-
Distinct modes of meltwater drainage and landform development beneath the last Barents Sea ice sheet
by: Calvin Shackleton, et al.
Published: (2023-04-01) -
Late Pleistocene to early Holocene environmental changes on Store Koldewey, coastal north-east Greenland
by: Martin Klug, et al.
Published: (2016-12-01) -
The Driving Mechanisms on Southern Ocean Upwelling Change during the Last Deglaciation
by: Wei Liu, et al.
Published: (2021-06-01) -
Lagged Linkage between the Kara–Barents Sea Ice and Early Summer Rainfall in Eastern China in Chinese CMIP6 Models
by: Huidi Yang, et al.
Published: (2023-04-01) -
Amplified wintertime Barents Sea warming linked to intensified Barents oscillation
by: Ziyi Cai, et al.
Published: (2022-01-01)