A new megalosaurid theropod dinosaur from the late Middle Jurassic (Callovian) of north-western Germany: implications for theropod evolution and faunal turnover in the Jurassic (project)

10.7934/p2368 ◽  
2016 ◽  
Author(s):  
W Rauhut ◽  
H Hübner ◽  
L Lanser
Keyword(s):  
Middle Jurassic ◽  
Theropod Dinosaur ◽  
Faunal Turnover ◽  
Western Germany ◽  
North Western

scholarly journals New theropod dinosaur teeth from the Middle Jurassic of the Isle of Skye, Scotland

2019 ◽  
Vol 55 (1) ◽  
pp. 7-19 ◽  
Author(s):  
Chloe M. E. Young ◽  
Christophe Hendrickx ◽  
Thomas J. Challands ◽  
Davide Foffa ◽  
Dugald A. Ross ◽  
...  
Keyword(s):  
Middle Jurassic ◽  
Theropod Dinosaur ◽  
Dinosaur Teeth ◽  
Isle Of Skye

scholarly journals Health status of free-ranging ring-necked pheasant chicks (Phasianus colchicus) in North-Western Germany

PLoS ONE ◽  
2020 ◽  
Vol 15 (6) ◽  
pp. e0234044 ◽  
Author(s):  
J. Liebing ◽  
I. Völker ◽  
N. Curland ◽  
P. Wohlsein ◽  
W. Baumgärtner ◽  
...  
Keyword(s):  
Health Status ◽  
Phasianus Colchicus ◽  
Western Germany ◽  
Free Ranging ◽  
North Western

Cosmogenic 36Cl in karst waters from Bunker Cave North Western Germany – A tool to derive local evapotranspiration?

2012 ◽  
Vol 86 ◽  
pp. 138-149 ◽  
Author(s):  
C. Münsterer ◽  
J. Fohlmeister ◽  
M. Christl ◽  
A. Schröder-Ritzrau ◽  
V. Alfimov ◽  
...  
Keyword(s):  
Karst Waters ◽  
Western Germany ◽  
North Western

scholarly journals Response of sediment to ice-sheet loading in northwestern Germany: effective stresses and glacier-bed stability

1997 ◽  
Vol 43 (145) ◽  
pp. 495-502 ◽  
Author(s):  
Jan A. Piotrowski ◽  
Anna M. Kraus
Keyword(s):  
Pore Water ◽  
Pore Water Pressure ◽  
Water Pressure ◽  
Ice Sheet ◽  
Bed Deformation ◽  
Pore Water Pressures ◽  
Sediment Consolidation ◽  
Western Germany ◽  
Bed Stability ◽  
North Western

AbstractLaboratory tests on sediment over-ridden by the last ice sheet in north-western Germany reveal very low ice-induced pre-consolidation and high palaeo-pore-water pressures. Sediment consolidation at the base of the glacier was largely controlled by hydraulic properties of the substratum. Generally low permeabilities of the bed caused sustained high pore-water pressure in over-ridden sediments close to the flotation point. This implies a serious possibility of hydraulic lifting of the ice sheet. It is believed that the reduced basal coupling limited the transformation of glacier shear stress on to the bed sediments, which is indicated by a lack of sedimentological evidence for widespread pervasive bed deformation. Ice motion was probably focused at the glacier sole by some combination of sliding and ploughing. However, isolated spots with deformation occur, so that the subglacial system in the study area can be characterized as a stable/deforming mosaic.

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