Late glacial and Holocene sedimentary environments of Quesnel Lake, British Columbia

Geomorphology ◽  
2012 ◽  
Vol 179 ◽  
pp. 186-196 ◽  
Author(s):  
Robert Gilbert ◽  
Joseph R. Desloges
Keyword(s):  
British Columbia ◽  
Late Glacial ◽  
Sedimentary Environments ◽  
Late Glacial And Holocene

scholarly journals Late glacial and Holocene sedimentation and investigation of fiord tsunami potential in lower Howe Sound, British Columbia

2014 ◽  
Author(s):  
L E Jackson ◽  
A Blais-Stevens ◽  
R L Hermanns ◽  
D P van Zeyl ◽  
D Stead ◽  
...  
Keyword(s):  
British Columbia ◽  
Late Glacial ◽  
Late Glacial And Holocene

Late-glacial and Holocene paleoceanography and sedimentary environments in the St. Anna Trough, Eurasian Arctic Ocean margin

1999 ◽  
Vol 146 (1-4) ◽  
pp. 229-249 ◽  
Author(s):  
Morten Hald ◽  
Vidar Kolstad ◽  
Leonid Polyak ◽  
Steven L. Forman ◽  
Frances A. Herlihy ◽  
...  
Keyword(s):  
Arctic Ocean ◽  
Late Glacial ◽  
Sedimentary Environments ◽  
Anna Trough ◽  
Late Glacial And Holocene

LATE GLACIAL AND HOLOCENE GLACIER FLUCTUATIONS IN THE CORDILLERA BLANCA, PERUVIAN ANDES

2016 ◽  
Author(s):  
Nathan Stansell ◽  
◽  
Donald T. Rodbell ◽  
Joseph M. Licciardi ◽  
Mark B. Abbott ◽  
...  
Keyword(s):  
Late Glacial ◽  
Cordillera Blanca ◽  
Peruvian Andes ◽  
Glacier Fluctuations ◽  
Late Glacial And Holocene

Mollusc successions reveal northward postglacial shifts of Alpine species ranges (Bohemian Massif, Czech Republic)

The Holocene ◽  
2021 ◽  
pp. 095968362110116
Author(s):  
Lucie Juřičková ◽  
Jakub Menšík ◽  
Jitka Horáčková ◽  
Vojen Ložek
Keyword(s):  
Czech Republic ◽  
Bohemian Massif ◽  
Late Glacial ◽  
Glacial Refugia ◽  
Land Snails ◽  
Glacial Refugium ◽  
Local Climate ◽  
The Alps ◽  
Species Groups ◽  
Late Glacial And Holocene

The Alps are an important hotspot of species diversity and endemism, as well as a presumed glacial refugium of several species’ groups including land snails. The recent ranges of Alpine endemics are well known, but their fluctuations during the postglacial period mirroring local climate changes are understudied. By analysing five Late Glacial and Holocene mollusc successions from two areas in the southernmost part of the Bohemian Massif (Czech Republic) situated about 100 km north of the Alps, we reveal details of these fluctuations. The Alpine endemic rocky dweller Chilostoma achates had reached the southern part of the Bohemian Massif already in the Late Glacial and disappeared in the Mid-Holocene canopy forest optimum. On the contrary, the northern boundaries of Alpine canopy forest epigeic snails extended further north than today at the turn of the Middle and Late-Holocene, pointing to a more favourable forest microclimate. The earliest known occurrences of several temperate canopy forest central European species, especially Causa holosericea and Discus perspectivus, imply the role of different areas in the Alps as their glacial refugia.

scholarly journals Late Glacial and Holocene plant cover in Węgliny, Lubsza Plain, south-west Poland, based on pollen analysis

2013 ◽  
Vol 53 (2) ◽  
pp. 191-233 ◽  
Author(s):  
Aleksandra Jurochnik ◽  
Dorota Nalepka
Keyword(s):  
Pollen Analysis ◽  
Plant Cover ◽  
Late Glacial ◽  
Anaerobic Sediments ◽  
The North ◽  
South West ◽  
Pollen Diagrams ◽  
Laacher See Tephra ◽  
Late Glacial And Holocene

ABSTRACT Late Glacial (since Oldest Dryas) and Holocene (to Subatlantic) changes of vegetation at the Węgliny site (south-west Poland) are reconstructed based mainly on pollen analysis of five cores from the palaeobasin (anaerobic sediments). The chronology of the described events is based on palynological comparison with the Lubsza Plain environs, based on LPAZs from several published pollen diagrams on 14C data, and multiple cryptotephra levels determined in the Węgliny profiles. The Węgliny record integrates well into the north European Holocene and Late Glacial biostratigraphic framework. The Węgliny site is the next (fourth) locality in Poland where the Laacher See Tephra (LST) horizon within the Allerød chronozone was identified.

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