Holocene paleoceanography and glacial history of the West Spitsbergen area, Euro-Arctic margin

Hald, Morten; Ebbesen, Hanne; Forwick, Matthias; Godtliebsen, Fred; Khomenko, Liza; Korsun, Sergei; Olsen, Lena Ringstad; Vorren, Tore O.

doi:10.1016/j.quascirev.2004.08.006

Cited by 141 publications

(190 citation statements)

References 33 publications

Supporting

Mentioning

169

Contrasting

Unclassified

Order By: Relevance

“…Cooling in the Fram Strait area during the late Holocene is reported at various locations and assigned reduced insolation (e.g. Hald et al, 2004;Müller et al, 2012;Rasmussen et al, 2012;Rigual-Hernández et al, 2017;Ślubowska-Woldengen et al, 2007;Werner et al, 2013). Although sea ice biomarkers suggest open waters during summer (Figs.…”

Section: Late Holocene (∼ 18-04 Ka) -Aftermath Of the Neoglaciationmentioning

confidence: 98%

“…JM98-845 (Rasmussen et al, 2012); 5. MD99-2304 (Hald et al, 2004); 6. MD99-2305 (Hald et al, 2004);7.…”

Section: Regional Settingmentioning

confidence: 99%

“…MD99-2304 (Hald et al, 2004); 6. MD99-2305 (Hald et al, 2004);7. JM02-440 (Ślubowska-Woldengen et al, 2007); 8.…”

Section: Regional Settingmentioning

confidence: 99%

“…During the HTM, increasing SSTs (based on planktic foraminiferal assemblages) were reconstructed at the western Svalbard continental slope (Hald et al, 2004), south of Spitsbergen at the Storfjorden slope (T. L. Rasmussen et al, 2014a), and at the western Barents slope (Sarnthein et al, 2003). Lacustrine records from NW Spitsbergen indicate maximum temperatures based on alkenones until ∼ 10.5 ka (van der Bilt et al, 2016).…”

Section: Early Holocene (∼ 117-78 Ka) -Amelioration Of Environmentamentioning

confidence: 99%

“…Woodfjorden and its trough constituted one of the main northern gateways for fast flowing ice streams that drained the northwestern sector of these ice sheets during the Last Glacial Maximum Ottesen et al, 2007). Whereas the Holocene and in part the late Weichselian have been relatively well documented off (south)western Svalbard (Hald et al, 2004;Jernas et al, 2013;Majewski et al, 2009;Rasmussen et al, 2007Rasmussen et al, , 2012; T. L. Rasmussen et al, 2014a;Sarnthein et al, 2003;Skirbekk et al, 2010;Ślubowska-Woldengen et al, 2007;Werner et al, 2011), palaeoceanographic records from northern Svalbard (Chauhan et al, 2014(Chauhan et al, , 2015Koç et al, 2002;Kubischta et al, 2011;Ślubowska et al, 2005) are still scarce (Fig. 1b).…”

Section: Introductionmentioning

confidence: 99%

See 4 more Smart Citations

Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation

et al. 2017

View full text Add to dashboard Cite

Abstract. Atlantic Water (AW) advection plays an important role in climatic, oceanographic and environmental conditions in the eastern Arctic. Situated along the only deep connection between the Atlantic and the Arctic oceans, the Svalbard Archipelago is an ideal location to reconstruct the past AW advection history and document its linkage with local glacier dynamics, as illustrated in the present study of a 275 cm long sedimentary record from Woodfjorden (northern Spitsbergen; water depth: 171 m) spanning the last ∼ 15 500 years.

show abstract

Section: Late Holocene (∼ 18-04 Ka) -Aftermath Of the Neoglaciationmentioning

confidence: 98%

“…JM98-845 (Rasmussen et al, 2012); 5. MD99-2304 (Hald et al, 2004); 6. MD99-2305 (Hald et al, 2004);7.…”

Section: Regional Settingmentioning

confidence: 99%

“…MD99-2304 (Hald et al, 2004); 6. MD99-2305 (Hald et al, 2004);7. JM02-440 (Ślubowska-Woldengen et al, 2007); 8.…”

Section: Regional Settingmentioning

confidence: 99%

Section: Early Holocene (∼ 117-78 Ka) -Amelioration Of Environmentamentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

See 3 more Smart Citations

Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation

et al. 2017

View full text Add to dashboard Cite

show abstract

Brine formation in relation to climate changes and ice retreat during the last 15,000 years in Storfjorden, Svalbard, 76–78°N

Rasmussen

Thomsen

2014

Paleoceanography

View full text Add to dashboard Cite

Storfjorden, Svalbard, is an area of intense brine formation. The brine is cold, dense, rich in oxygen and CO 2 , and has reduced pH. Storfjorden is unique because it contains well-preserved agglutinated foraminifera dating back to the beginning of the last deglaciation. We have investigated the distribution of calcareous and agglutinated benthic foraminifera, benthic oxygen and carbon isotopes, calcium carbonate, total organic carbon, and ice-rafted debris in five cores from Storfjorden comprising the Holocene and the deglaciation. The purpose of the study is to reconstruct brine formation in the past under different climate scenarios. The data indicate that in Storfjorden the ratio of agglutinated to calcareous benthic foraminifera can be taken as a measure of the strength of brine formation. The foraminiferal data, which are supported by stable isotopes, degree of fragmentation, and geochemical parameters, signify that brine formation intensified during cold periods and weakened during warm periods.

show abstract

From everywhere all at once: Several colonization routes available to Svalbard in the early Holocene

Brožová

Bolstad²,

Seregin

et al. 2023

Ecology and Evolution

View full text Add to dashboard Cite

show abstract

Holocene paleoceanography and glacial history of the West Spitsbergen area, Euro-Arctic margin

Cited by 141 publications

References 33 publications

Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation

Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation

Brine formation in relation to climate changes and ice retreat during the last 15,000 years in Storfjorden, Svalbard, 76–78°N

From everywhere all at once: Several colonization routes available to Svalbard in the early Holocene

Contact Info

Product

Resources

About