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• W3201105245 endingPage "4380" @default.
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• W3201105245 abstract "Abstract. The Petermann 2015 expedition to Petermann Fjord and adjacent Hall Basin recovered a transect of cores, extending from Nares Strait to underneath the 48 km long ice tongue of Petermann glacier, offering a unique opportunity to study ice–ocean–sea ice interactions at the interface of these realms. First results suggest that no ice tongue existed in Petermann Fjord for large parts of the Holocene, raising the question of the role of the ocean and the marine cryosphere in the collapse and re-establishment of the ice tongue. Here we use a multi-proxy approach (sea-ice-related biomarkers, total organic carbon and its carbon isotopic composition, and benthic and planktonic foraminiferal abundances) to explore Holocene sea ice dynamics at OD1507-03TC-41GC-03PC in outer Petermann Fjord. Our results are in line with a tight coupling of the marine and terrestrial cryosphere in this region and, in connection with other regional sea ice reconstructions, give insights into the Holocene evolution of ice arches and associated landfast ice in Nares Strait. The late stages of the regional Holocene Thermal Maximum (6900–5500 cal yr BP) were marked by reduced seasonal sea ice concentrations in Nares Strait and the lack of ice arch formation. This was followed by a transitional period towards Neoglacial cooling from 5500–3500 cal yr BP, where a southern ice arch might have formed, but an early seasonal breakup and late formation likely caused a prolonged open water season and enhanced pelagic productivity in Nares Strait. Between 3500 and 1400 cal yr BP, regional records suggest the formation of a stable northern ice arch only, with a short period from 2500–2100 cal yr BP where a southern ice arch might have formed intermittently in response to atmospheric cooling spikes. A stable southern ice arch, or even double arching, is also inferred for the period after 1400 cal yr BP. Thus, both the inception of a small Petermann ice tongue at ∼ 2200 cal yr BP and its rapid expansion at ∼ 600 cal yr BP are preceded by a transition towards a southern ice arch regime with landfast ice formation in Nares Strait, suggesting a stabilizing effect of landfast sea ice on Petermann Glacier." @default.
• W3201105245 created "2021-09-27" @default.
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• W3201105245 date "2021-09-10" @default.
• W3201105245 modified "2023-09-26" @default.
• W3201105245 title "Holocene sea-ice dynamics in Petermann Fjord in relation to ice tongue stability and Nares Strait ice arch formation" @default.
• W3201105245 cites W1429673265 @default.
• W3201105245 cites W1491347125 @default.
• W3201105245 cites W1505956466 @default.
• W3201105245 cites W1641849691 @default.
• W3201105245 cites W1757514996 @default.
• W3201105245 cites W1941837661 @default.
• W3201105245 cites W1964328088 @default.
• W3201105245 cites W1964909389 @default.
• W3201105245 cites W1967214983 @default.
• W3201105245 cites W1974632989 @default.
• W3201105245 cites W1976919944 @default.
• W3201105245 cites W1978912155 @default.
• W3201105245 cites W1979518614 @default.
• W3201105245 cites W1986316608 @default.
• W3201105245 cites W1986456129 @default.
• W3201105245 cites W1988287153 @default.
• W3201105245 cites W2002784775 @default.
• W3201105245 cites W2004183810 @default.
• W3201105245 cites W2009435259 @default.
• W3201105245 cites W2011749856 @default.
• W3201105245 cites W2012623757 @default.
• W3201105245 cites W2013234742 @default.
• W3201105245 cites W2014048805 @default.
• W3201105245 cites W2016533670 @default.
• W3201105245 cites W2021824008 @default.
• W3201105245 cites W2026087292 @default.
• W3201105245 cites W2030881763 @default.
• W3201105245 cites W2035511167 @default.
• W3201105245 cites W2040113174 @default.
• W3201105245 cites W2046988120 @default.
• W3201105245 cites W2048434240 @default.
• W3201105245 cites W2052210986 @default.
• W3201105245 cites W2052281849 @default.
• W3201105245 cites W2054307300 @default.
• W3201105245 cites W2057907380 @default.
• W3201105245 cites W2059175769 @default.
• W3201105245 cites W2059513284 @default.
• W3201105245 cites W2059900540 @default.
• W3201105245 cites W2065567439 @default.
• W3201105245 cites W2066980677 @default.
• W3201105245 cites W2069361996 @default.
• W3201105245 cites W2073255904 @default.
• W3201105245 cites W2076729581 @default.
• W3201105245 cites W2077764993 @default.
• W3201105245 cites W2078574678 @default.
• W3201105245 cites W2079341590 @default.
• W3201105245 cites W2081840645 @default.
• W3201105245 cites W2092188312 @default.
• W3201105245 cites W2095255457 @default.
• W3201105245 cites W2103188186 @default.
• W3201105245 cites W2106585957 @default.
• W3201105245 cites W2108808592 @default.
• W3201105245 cites W2109173236 @default.
• W3201105245 cites W2115870595 @default.
• W3201105245 cites W2147787753 @default.
• W3201105245 cites W2149435696 @default.
• W3201105245 cites W2149845293 @default.
• W3201105245 cites W2154666809 @default.
• W3201105245 cites W2156567817 @default.
• W3201105245 cites W2163558759 @default.
• W3201105245 cites W2168902415 @default.
• W3201105245 cites W2171339030 @default.
• W3201105245 cites W2177254452 @default.
• W3201105245 cites W2215848034 @default.
• W3201105245 cites W2289736227 @default.
• W3201105245 cites W2315085235 @default.
• W3201105245 cites W2320124179 @default.
• W3201105245 cites W2337598496 @default.
• W3201105245 cites W2405649852 @default.
• W3201105245 cites W2549832170 @default.
• W3201105245 cites W2566694496 @default.
• W3201105245 cites W2569039531 @default.
• W3201105245 cites W2581664766 @default.
• W3201105245 cites W2584537188 @default.
• W3201105245 cites W2592292043 @default.
• W3201105245 cites W2594817380 @default.
• W3201105245 cites W2604701148 @default.
• W3201105245 cites W2614494230 @default.
• W3201105245 cites W2618911005 @default.
• W3201105245 cites W2727128072 @default.
• W3201105245 cites W2747264389 @default.
• W3201105245 cites W2792127876 @default.
• W3201105245 cites W2805202119 @default.
• W3201105245 cites W2892275439 @default.

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