Detectable land use impact on methanotrophs and methanogens in kettle hole sediments but not on net methane production potentials. [PDF]
Kynast D +5 more
europepmc +1 more source
Insights to the taxonomy and phylogeny of the genus Ptilagrostis worldwide (Poaceae, Stipeae) with a key to species identification, checklist and outlines for further studies. [PDF]
Krzempek M, Klichowska E, Nobis M.
europepmc +1 more source
Diversity and biogeography of the bacterial microbiome in glacier-fed streams. [PDF]
Ezzat L +19 more
europepmc +1 more source
Automated determination of transport and depositional environments in sand and sandstones. [PDF]
Hasson M, Marvin MC, Lapôtre MGA.
europepmc +1 more source
Reproductive Performance of the Alpine Plant Species Ranunculus kuepferi in a Climatic Elevation Gradient: Apomictic Tetraploids Do Not Show a General Fitness Advantage over Sexual Diploids. [PDF]
Ladinig U +3 more
europepmc +1 more source
Terminal moraines in the fjord basins of sub-Antarctic South Georgia
Sub-Antarctic South Georgia (54° 17′ S, 36° 30′ W, 3755 km2) is a large heavily glacierized island that is 170 km long, 39 km wide and rises to elevations of 2934 m. The island has extensive evidence of past glacial expansion with moraines preserved on land (Bentley et al. 2007), in the fjords (Hodgson et al. 2014) and in glacial troughs that extend 60–
Graham, A.G.C., Hodgson, D.A.
openaire +4 more sources
The Late Devensian terminal moraine ridge at Garret Hill, Stiffkey valley, north Norfolk, England
SUMMARY Glacial stratigraphy and ice-marginal processes within the limit of the Late Devensian Glaciation in eastern England were investigated at Garret Hill, situated on the eastern flank of the Stiffkey valley, north Norfolk. Glacial sediments are divided into four lithofacies units.
S. M. Pawley, I. Candy, S. J. Booth
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Abstract The formation of terminal moraines dating from glacier advances during the A.D. 1990s was investigated at six temperate glaciers in the Jostedalsbreen and Jotunheimen regions of southern Norway. Morphological and sedimentological information was analysed and combined with detailed observations, photographic evidence, and length variation ...
Stefan Winkler, John A. Matthews
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