Upper Late Weichselian lithostratigraphy in western Skåne, southernmost Sweden

Ringberg, Bertil

doi:10.1080/11035898909453130

Cited by 26 publications

(22 citation statements)

References 22 publications

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“…in accordance with the above-described fan-shaped arrangement directions in Skåne), while the younger phases of the Weichselian are associated with the operation of the paleo-ice stream flowing from the east and southeast (see e.g. Ringberg, 1989;Lindstr€ om, 1991;Mattson, 1997;Kjaer et al, 2003;Larsen et al, 2009;Anjar et al, 2014). The inflow of the ice from the NE was slow and was accompanied by a strong erosion of the substrate, as opposed to the subsequent fast moving stream (Kjaer et al, 2003).…”

Section: Ice Flow Directionsmentioning

confidence: 59%

“…However, there is evidence of ice flow from the north and north-west from SW Fennoscandia, associated with the period immediately preceding the Late Weichselian, or with older ice sheets (cf. Ringberg, 1989;Lindstr€ om, 1991;Mattson, 1997). What can therefore be assumed is a multi-stage transport of the rocks from Bornholm and Skåne far to the east.…”

Section: Ice Flow Directionsmentioning

confidence: 98%

See 1 more Smart Citation

The Late Weichselian glacial record in northern Poland: A new look at debris transport routes by the Fennoscandian Ice Sheet

Woźniak

Czubla

2015

Quaternary International

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Section: Ice Flow Directionsmentioning

confidence: 59%

Section: Ice Flow Directionsmentioning

confidence: 98%

The Late Weichselian glacial record in northern Poland: A new look at debris transport routes by the Fennoscandian Ice Sheet

Woźniak

Czubla

2015

Quaternary International

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“…It has been a matter of dispute for some decades and i s still a topic of discussion (e.g. Lagerlund, 1977Lagerlund, , 1980Lagerlund, , 1987Ringberg, 1988Ringberg, , 1989. According to Lagerlund's hypothetical, but highly sensitive and dynamic model, three advances (surges) and subsequent collapses of ice-domes in the southwest preceded a more continuous deglaciation after 13000 yr BP.…”

Section: Chronology Deglaciation and Sea-level Changesmentioning

confidence: 99%

Late Weichselian environmental change in southern Sweden and Denmark

Berglund

Björck

Lemdahl

et al. 1994

J Quaternary Science

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A synthesis is presented of the environmental and climatic variations that are inferred to have occurred in southern Sweden (up to latitude 59"N) and Denmark during the Weichselian Late-glacial (1 4-9 kaBP). The chronology and characteristics of the main phases of deglaciation, sea-level change, periglacial activity, soil development, vegetation cover and climate change are summarised. A curve representing the main changes in temperature, including quantitative estimates based upon beetle data and using the 'mutual climatic range' method, is presented.Journal of Quaternary Science

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“…During the Weichselian glaciation (about 13 700 BP), polar cod and its main predator, ringed seal (Phoca hispida), were abundant as far to the south as the southernmost parts of Scandinavia indicating an arctic sea ice environment (Ringberg 1989). Based on fossil records, polar cod disappeared from northern Norway about 10 000 BP and it was succeeded by boreal gadoid fish species (Gadidae) such as Norway pout, Trisopterus esmarkii, and Atlantic cod, Gadus morhua (Gaemers & Vorren 1985).…”

Section: Discussionmentioning

confidence: 99%