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Record #197558:
Climate variability in west Greenland during the past 1500 years: evidence from a high-resolution marine palynological record from Disko Bay / Sofia Ribeiro, and 3 others.
Title: | Climate variability in west Greenland during the past 1500 years: evidence from a high-resolution marine palynological record from Disko Bay / Sofia Ribeiro, and 3 others. |
Author(s): | Ribeiro, Sofia. |
Date: | 2012. |
In: | Boreas. (2012.), Vol. 41(1) (2012) |
Abstract: | Documents Late-Holocene climate variability in west Greenland as inferred from marine sediment record from outer Disko Bay. Uses organic-walled dinoflagellate cysts and other palynomorphs to reconstruct environmental changes in area through last c. 1500 years at 30-40-years resolution. Identifies sea ice cover and primary productivity as two main factors driving dinoflagellate cyst community changes over time. Data provide evidence for opposite climate trend in west Greenland relative to that of NE Atlantic region from c. AD 500-1050. |
Notes: | Boreas. Vol. 41(1) :68-83 (2012). |
Keywords: | 551.326 -- Floating ice. 551.352/.353 -- Marine sediments, deep sea. 551.583 -- Climatic changes. 551.583.3 -- Climatic changes, Quaternary. 574.55 -- Productivity, aquatic ecology. 581.081.3 -- Pollen analysis. D -- Atmospheric sciences. (*3) -- Arctic regions. (*38) -- Greenland. (*384) -- West Greenland. |
SPRI record no.: | 197558 |
LDR 01784naa#a2200000#a#4500 001 SPRI-197558 005 20230930011830.0 007 ta 008 230930s2012####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-197558 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aRibeiro, Sofia. 245 10 ‡aClimate variability in west Greenland during the past 1500 years :‡bevidence from a high-resolution marine palynological record from Disko Bay /‡cSofia Ribeiro, and 3 others. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2012. 300 ## ‡ap. 68-83 :‡bill., diags., tables, map. 500 ## ‡aBoreas. Vol. 41(1) :68-83 (2012). 520 3# ‡aDocuments Late-Holocene climate variability in west Greenland as inferred from marine sediment record from outer Disko Bay. Uses organic-walled dinoflagellate cysts and other palynomorphs to reconstruct environmental changes in area through last c. 1500 years at 30-40-years resolution. Identifies sea ice cover and primary productivity as two main factors driving dinoflagellate cyst community changes over time. Data provide evidence for opposite climate trend in west Greenland relative to that of NE Atlantic region from c. AD 500-1050. 530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1502-3885.2011.00216.x‡uhttps://dx.doi.org/10.1111/j.1502-3885.2011.00216.x 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.352/.353 -- Marine sediments, deep sea.‡2udc 650 07 ‡a551.583 -- Climatic changes.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡a574.55 -- Productivity, aquatic ecology.‡2udc 650 07 ‡a581.081.3 -- Pollen analysis.‡2udc 650 07 ‡aD -- Atmospheric sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*38) -- Greenland.‡2udc 651 #7 ‡a(*384) -- West Greenland.‡2udc 773 0# ‡7nnas ‡tBoreas. ‡gVol. 41(1) (2012) ‡wSPRI-56035 916 ## ‡a2012/01/31 -- JW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230930 ‡bJW