Faunal and taphonomic analyses of a Late Pleistocene bird-bone assemblage from a cave deposit in north-west Hungary

Geobios ◽  
2008 ◽  
Vol 41 (1) ◽  
pp. 79-90 ◽  
Author(s):  
Erika Gál
Keyword(s):  
Late Pleistocene ◽  
North West ◽  
Cave Deposit

scholarly journals Thorough assessment of DNA preservation from fossil bone and sediments excavated from a late Pleistocene–Holocene cave deposit on Kangaroo Island, South Australia

2014 ◽  
Vol 84 ◽  
pp. 56-64 ◽  
Author(s):  
Dalal Haouchar ◽  
James Haile ◽  
Matthew C. McDowell ◽  
Dáithí C. Murray ◽  
Nicole E. White ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
South Australia ◽  
Fossil Bone ◽  
Dna Preservation ◽  
Cave Deposit

Late Pleistocene hydroclimatic variabilities in arid north‐west China: geochemical evidence from Balikun Lake, eastern Tienshan, China

2021 ◽  
Vol 36 (3) ◽  
pp. 415-425
Author(s):  
Yongtao Zhao ◽  
Cheng‐Bang An ◽  
Aifeng Zhou ◽  
Xiaonan Zhang ◽  
Jiaju Zhao ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
West China ◽  
North West ◽  
Geochemical Evidence

scholarly journals Oral health in Late Pleistocene and Holocene North West Africa

2018 ◽  
Vol 22 ◽  
pp. 392-400 ◽  
Author(s):  
Isabelle De Groote ◽  
Jacob Morales ◽  
Louise Humphrey
Keyword(s):  
Oral Health ◽  
West Africa ◽  
Late Pleistocene ◽  
North West

scholarly journals Late Pleistocene to Holocene palaeoenvironmental variability in the north-west Spanish mountains: insights from a source-to-sink environmental magnetic study of Lake Sanabria

2015 ◽  
Vol 30 (3) ◽  
pp. 222-234 ◽  
Author(s):  
VIOLETA BORRUEL-ABADÍA ◽  
MIRIAM GÓMEZ-PACCARD ◽  
JUAN C. LARRASOAÑA ◽  
MAYTE RICO ◽  
BLAS VALERO-GARCÉS ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
Magnetic Study ◽  
North West ◽  
The North ◽  
Source To Sink ◽  
Late Pleistocene To Holocene

Late Pleistocene and Holocene Reef Growth in Southern Kimberley, North West Australia

2015 ◽  
Author(s):  
Giada Bufarale ◽  
Lindsay Collins ◽  
Michael O'Leary ◽  
Alexandra Stevens ◽  
Moataz Kordi ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
Reef Growth ◽  
North West ◽  
Holocene Reef

Palaeolithic Implements from Kirmington, Lincolnshire, and their relation to the 100-foot raised beach of Late Pleistocene Times

1931 ◽  
Vol 11 (3) ◽  
pp. 262-272 ◽  
Author(s):  
J. P. T. Burchell
Keyword(s):  
Late Pleistocene ◽  
Late Glacial ◽  
Upper Palaeolithic ◽  
Similar Nature ◽  
East Anglia ◽  
North West ◽  
North East ◽  
Boulder Clay

Last year I described before the Society a series of flint implements of Upper Palaeolithic (Upper Mousterian-Aurignacian) facies discovered by me in Yorkshire at the base of, and passing up into, a deposit considered by Lamplugh to resemble a weathered Boulder clay and classed by him as of Late Glacial Age. The geological aspects of these archaeological finds I have dealt with fully in a paper read subsequently to the Prehistoric Society of East Anglia. Both papers, however, were complementary to one read by J.Reid Moir on archaeological discoveries of a similar nature made by him in north-west Norfolk in the Brown Boulder clay. With the objects of obtaining confirmation of Lamplugh's geological opinion and of bridging the gap between north-west Norfolk and Yorkshire, I decided to investigate the glacial sequence in north-east Lincolnshire, choosing Kirmington as a centre.

scholarly journals Revisiting Late Pleistocene glacier dynamics north-west of the Feldberg, southern Black Forest, Germany

2020 ◽  
Vol 69 (1) ◽  
pp. 61-87
Author(s):  
Felix Martin Hofmann ◽  
Florian Rauscher ◽  
William McCreary ◽  
Jan-Paul Bischoff ◽  
Frank Preusser
Keyword(s):  
Late Pleistocene ◽  
Remote Sensing Data ◽  
Black Forest ◽  
Air Masses ◽  
North West ◽  
Ice Cap ◽  
Last Glaciation ◽  
The Alps ◽  
Area North ◽  
Glacial Landforms

Abstract. The southern Black Forest was temporarily covered by a ∼1000 km2 large ice cap during the Late Pleistocene. However, during the last glaciation maximum in the Alps the atmospheric circulation over Europe was presumably characterised by the advection of humid air masses from the Mediterranean Sea. As a consequence, the ice cap of the Black Forest was likely in a leeward position due to its location north of the Alps. This raises the question of whether it reached its last maximum extent simultaneously with the glaciers in the Alps. As modern dating techniques have hitherto not been applied to the southern Black Forest, the timing of the last local glaciation maximum remains poorly constrained. As a first step towards an independent regional glacier chronology, we present a critical re-examination of glacial landforms in the area north-west of the highest summit of the Black Forest (Feldberg, 1493 m a.s.l.). It relies on both the analysis of remote sensing data and field mapping. The review of previous studies highlights important disagreements regarding the location of ice-marginal positions and their correlation. In addition, our findings challenge earlier studies on the glaciation of the Black Forest: some previously described ice-marginal positions could not be confirmed, whereas some of the newly identified moraines are described for the first time. This highlights the need for detailed geomorphological investigations prior to the application of geochronological methods. A multi-ridged series of terminal moraines in one of the studied valleys, Sankt Wilhelmer Tal, is proposed as the main target for future dating. Due to discrepancies with earlier studies, future efforts should reinvestigate other key areas related to the last glaciation of the southern Black Forest.

Availability of fossiliferous sediment from the Red Hills Road Cave (late Pleistocene), Jamaica

1997 ◽  
Vol 71 (2) ◽  
pp. 351-351 ◽  
Author(s):  
Stephen K. Donovan
Keyword(s):  
Late Pleistocene ◽  
Marine Crustaceans ◽  
Precise Locality ◽  
The Caribbean ◽  
Locality Information ◽  
Cave Deposit ◽  
Red Hills

The purpose of this note is to record the availability for research of highly fossiliferous sediment from a late Pleistocene terrestrial deposit in the Caribbean. The Red Hills Road cave in the parish of St. Andrew, northwest of Kingston, Jamaica (for more precise locality information, see Donovan et al., 1995, p. 12-15) is a late Pleistocene, essentially unstratified, cave deposit. The terrestrial fauna from this site includes diverse vertebrates (Savage, 1990; D.A. McFarlane and R.D.E. MacPhee, research in progress) and gastropods, associated with rare arthropods including millipedes (Donovan and Veltkamp, 1994), isopods, ostracodes and claws of non-marine crustaceans (J. S. H. Collins, research in progress).

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