Results 51 to 60 of about 1,544 (188)
Abstract Recovering the patterns of glacial erosion over time is key to understanding feedbacks between climate and tectonic processes. Glacial erosion rates have been shown to systematically increase worldwide toward the present since the late Cenozoic, a behavior interpreted as the response of glaciers to a cooling and increasingly variable climate ...
A. Fedotova, M. B. Magnani
wiley +1 more source
Negyedidőszaki szárazföldi- és mélytengeri üledékek korrelációja Duna-menti löszök komplex sztratigráfiai vizsgálata alapján = Correlation of terrestrial and deep-sea Quaternary deposits on the basis of complex stratigraphic investigation into loesses along the Danube [PDF]
Őskörnyezet-változásokat és a fejlődéstörténetre vonatkozó változásokat vizsgáltunk Duna menti és vízrendszeréhez tartozó löszök típusfeltárásai alapján.
Balogh, János +3 more
core
Sandy loess deposits in the Fläming ridge (Brandenburg, Germany) were analysed with respect to their composition, depositional age and distribution in the landscape. They most likely originate in the lowlands to the north and were deposited during the late MIS 2 (19–14 ka), in analogy to loess deposits found further west and south.
Fabian Kirsten +7 more
wiley +1 more source
Abstract The soil mantle of the tropical karstic landscapes of Southern Mexico was shaped by specific processes of pedogenesis and long‐term human impacts of ancient Maya agriculture. To understand the interaction between natural and human‐induced soil‐forming processes in the calcareous mountains of Chiapas state, we studied soil toposequences around ...
P. García‐Ramírez +9 more
wiley +1 more source
Facies changes, sedimentary environments and sequence stratigraphy of the lower Carboniferous deposits in the Kalmard area, Central Iran, Member D of Gachal formation [PDF]
Lower Carboniferous deposits of Kalmard area identified with informal Gachal formation which in different outcrops have different lithologic features. This formation is consists of four members A, B, C and D that predominantly consists of carbonate and ...
Mohammadnabi Gorgij +1 more
doaj +1 more source
The mineralogical composition of calcium and calcium-magnesium carbonate pedofeatures of calcareous soils in the European prairie ecodivision in Hungary [PDF]
There is little data on the mineralogy of carbonate pedofeatures in the calcareous soils in Hungary which belong to the European prairie ecodivision. The aim of the present study is to enrich these data.
Amundson R.G. +59 more
core +1 more source
Abstract To date, the most complete paleolake‐level reconstructions for the late Pleistocene water bodies that once occupied the Dead Sea depression have been based on the combination of dating of lake sediments and terrestrial materials. However, despite these major accomplishments, there is still limited spatial control regarding the water levels ...
Julius Jara‐Muñoz +12 more
wiley +1 more source
Abstract Investigating rock‐uplift variations in time and space provides insights into the processes driving mountain‐belt evolution. The Apennine Mountains of Italy underwent substantial Quaternary rock uplift that shaped the present‐day topography. Here, we present linear river‐profile inversions for 28 catchments draining the eastern flank of the ...
S. Racano +5 more
wiley +1 more source
ABSTRACT Three hundred forty‐one radiocarbon dates from the Groningen radiocarbon database are compiled in this study. They show for the first time that organic sediment samples from the eastern Netherlands and mammal bones from Doggerland reflect shifts in the presence and the density of vegetation (food for herbivores) and mammal biomass during the ...
B. Van Geel +3 more
wiley +1 more source
Circum-Mediterranean Neogene (Miocene and Pliocene) marine-continental chronologic correlations of European mammal units [PDF]
This paper is an update of Steininger et al. 1989. It is mainly concerned with the chronologic correlation of the Miocene and Pliocene European Mammal Biozonations, the "European Neogene Mammal Faunal Zones" (MN zones, for discussion see Steininger et al.
Agusti, J. +5 more
core +2 more sources

