FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000202990> ?p ?o ?g. }

• W2000202990 endingPage "435" @default.
• W2000202990 startingPage "435" @default.
• W2000202990 abstract "Research Article| May 01, 2002 Benthic foraminiferal record of Holocene deep-water evolution in the Palmer Deep, western Antarctic Peninsula S.E. Ishman; S.E. Ishman 1Department of Geology, Southern Illinois University, Carbondale, Illinois 62901-4324, USA Search for other works by this author on: GSW Google Scholar M.R. Sperling M.R. Sperling 2Institute and Museum of Geology and Paleontology, Sigwartstrasse 10, Tübingen, Germany Search for other works by this author on: GSW Google Scholar Geology (2002) 30 (5): 435–438. https://doi.org/10.1130/0091-7613(2002)030<0435:BFROHD>2.0.CO;2 Article history received: 09 Sep 2001 rev-recd: 27 Dec 2001 accepted: 14 Jan 2002 first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation S.E. Ishman, M.R. Sperling; Benthic foraminiferal record of Holocene deep-water evolution in the Palmer Deep, western Antarctic Peninsula. Geology 2002;; 30 (5): 435–438. doi: https://doi.org/10.1130/0091-7613(2002)030<0435:BFROHD>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Benthic foraminiferal data from Ocean Drilling Program Site 1098 indicate significant changes in deep-water conditions of the Palmer Deep, western Antarctic Peninsula margin, throughout the Holocene (13 ka to present). The earliest Holocene represents a period of transition from the Last Glacial Maximum (LGM). Cold bottom waters, similar to saline shelf water (SSW), dominated the middle Holocene. The late Holocene in the Palmer Deep has been characterized by alternating dominance of circumpolar deep water (CDW) and saline shelf water. These changes have global oceanographic and climatic implications. We suggest that the middle Holocene bottom-water record, in the absence of circumpolar deep water on the western Antarctic Peninsula shelf, indicates high saline shelf water production and/or weakened circumpolar deep water production during the middle Holocene climatic optimum. The late Holocene benthic foraminiferal record indicates rapidly fluctuating sea-ice conditions and may indicate a teleconnection between the South Pacific and Southern Ocean, thus having implications related to the Southern Oscillation Index. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2000202990 created "2016-06-24" @default.
• W2000202990 creator A5001726297 @default.
• W2000202990 creator A5016730121 @default.
• W2000202990 date "2002-01-01" @default.
• W2000202990 modified "2023-10-18" @default.
• W2000202990 title "Benthic foraminiferal record of Holocene deep-water evolution in the Palmer Deep, western Antarctic Peninsula" @default.
• W2000202990 cites W1501961051 @default.
• W2000202990 cites W1516943049 @default.
• W2000202990 cites W1540587825 @default.
• W2000202990 cites W1556773719 @default.
• W2000202990 cites W1564525918 @default.
• W2000202990 cites W1588188200 @default.
• W2000202990 cites W1592353562 @default.
• W2000202990 cites W1592912056 @default.
• W2000202990 cites W1617308574 @default.
• W2000202990 cites W1984826863 @default.
• W2000202990 cites W1989199622 @default.
• W2000202990 cites W1990947265 @default.
• W2000202990 cites W1995117601 @default.
• W2000202990 cites W2002300998 @default.
• W2000202990 cites W2004130518 @default.
• W2000202990 cites W2008875043 @default.
• W2000202990 cites W2013690179 @default.
• W2000202990 cites W2016737438 @default.
• W2000202990 cites W2030566361 @default.
• W2000202990 cites W2033505671 @default.
• W2000202990 cites W2058718049 @default.
• W2000202990 cites W2065712243 @default.
• W2000202990 cites W2076254583 @default.
• W2000202990 cites W2076839274 @default.
• W2000202990 cites W2084152834 @default.
• W2000202990 cites W2088147665 @default.
• W2000202990 cites W2091161534 @default.
• W2000202990 cites W2093312377 @default.
• W2000202990 cites W2094971954 @default.
• W2000202990 cites W2096919365 @default.
• W2000202990 cites W2104807682 @default.
• W2000202990 cites W2130256070 @default.
• W2000202990 cites W2167926476 @default.
• W2000202990 cites W2332133158 @default.
• W2000202990 cites W4240784109 @default.
• W2000202990 doi "https://doi.org/10.1130/0091-7613(2002)030<0435:bfrohd>2.0.co;2" @default.
• W2000202990 hasPublicationYear "2002" @default.
• W2000202990 type Work @default.
• W2000202990 sameAs 2000202990 @default.
• W2000202990 citedByCount "40" @default.
• W2000202990 countsByYear W20002029902012 @default.
• W2000202990 countsByYear W20002029902013 @default.
• W2000202990 countsByYear W20002029902014 @default.
• W2000202990 countsByYear W20002029902015 @default.
• W2000202990 countsByYear W20002029902016 @default.
• W2000202990 countsByYear W20002029902017 @default.
• W2000202990 countsByYear W20002029902018 @default.
• W2000202990 countsByYear W20002029902019 @default.
• W2000202990 countsByYear W20002029902020 @default.
• W2000202990 countsByYear W20002029902021 @default.
• W2000202990 countsByYear W20002029902022 @default.
• W2000202990 countsByYear W20002029902023 @default.
• W2000202990 crossrefType "journal-article" @default.
• W2000202990 hasAuthorship W2000202990A5001726297 @default.
• W2000202990 hasAuthorship W2000202990A5016730121 @default.
• W2000202990 hasConcept C100970517 @default.
• W2000202990 hasConcept C111368507 @default.
• W2000202990 hasConcept C123588078 @default.
• W2000202990 hasConcept C127313418 @default.
• W2000202990 hasConcept C140345934 @default.
• W2000202990 hasConcept C151730666 @default.
• W2000202990 hasConcept C161191863 @default.
• W2000202990 hasConcept C166957645 @default.
• W2000202990 hasConcept C199360897 @default.
• W2000202990 hasConcept C205649164 @default.
• W2000202990 hasConcept C2778447006 @default.
• W2000202990 hasConcept C2778805511 @default.
• W2000202990 hasConcept C2780368712 @default.
• W2000202990 hasConcept C41008148 @default.
• W2000202990 hasConcept C83042747 @default.
• W2000202990 hasConcept C95457728 @default.
• W2000202990 hasConceptScore W2000202990C100970517 @default.
• W2000202990 hasConceptScore W2000202990C111368507 @default.
• W2000202990 hasConceptScore W2000202990C123588078 @default.
• W2000202990 hasConceptScore W2000202990C127313418 @default.
• W2000202990 hasConceptScore W2000202990C140345934 @default.
• W2000202990 hasConceptScore W2000202990C151730666 @default.
• W2000202990 hasConceptScore W2000202990C161191863 @default.
• W2000202990 hasConceptScore W2000202990C166957645 @default.
• W2000202990 hasConceptScore W2000202990C199360897 @default.
• W2000202990 hasConceptScore W2000202990C205649164 @default.
• W2000202990 hasConceptScore W2000202990C2778447006 @default.
• W2000202990 hasConceptScore W2000202990C2778805511 @default.
• W2000202990 hasConceptScore W2000202990C2780368712 @default.
• W2000202990 hasConceptScore W2000202990C41008148 @default.
• W2000202990 hasConceptScore W2000202990C83042747 @default.
• W2000202990 hasConceptScore W2000202990C95457728 @default.
• W2000202990 hasIssue "5" @default.
• W2000202990 hasLocation W20002029901 @default.
• W2000202990 hasOpenAccess W2000202990 @default.
• W2000202990 hasPrimaryLocation W20002029901 @default.

• next