Loess in Pleistocene periglacial slope deposits and Holocene colluvium of European low mountain ranges: Mixing processes and spatial variations

CATENA ◽  
2021 ◽  
Vol 207 ◽  
pp. 105666
Author(s):  
Fei Yang ◽  
Gan-Lin Zhang ◽  
Volker Karius ◽  
Daniela Sauer
Forests ◽  
2021 ◽  
Vol 12 (7) ◽  
pp. 924
Author(s):  
Astrid Stobbe ◽  
Maren Gumnior

In the Central German Uplands, Fagus sylvatica and Picea abies have been particularly affected by climate change. With the establishment of beech forests about 3000 years ago and pure spruce stands 500 years ago, they might be regarded as ‘neophytes’ in the Hessian forests. Palaeoecological investigations at wetland sites in the low mountain ranges and intramontane basins point to an asynchronous vegetation evolution in a comparatively small but heterogenous region. On the other hand, palynological data prove that sustainably managed woodlands with high proportions of Tilia have been persisting for several millennia, before the spread of beech took place as a result of a cooler and wetter climate and changes in land management. In view of increasingly warmer and drier conditions, Tilia cordata appears especially qualified to be an important silvicultural constituent of the future, not only due to its tolerance towards drought, but also its resistance to browsing, and the ability to reproduce vegetatively. Forest managers should be encouraged to actively promote the return to more stress-tolerant lime-dominated woodlands, similar to those that existed in the Subboreal chronozone.


2001 ◽  
Vol 5 (3) ◽  
pp. 367-378 ◽  
Author(s):  
C. Alewell ◽  
M. Armbruster ◽  
J. Bittersohl ◽  
C. D. Evans ◽  
H. Meesenburg ◽  
...  

Abstract. The reversal of freshwater acidification in the low mountain ranges of Germany is of public, political and scientific concern, because these regions are near natural ecosystems and function as an important drinking water supply. The aim of this study was to evaluate the status and trends of acidification reversal after two decades of reduced anthropogenic deposition in selected freshwaters of the low mountain ranges in the Harz, the Fichtelgebirge, the Bavarian Forest, the Spessart and the Black Forest. In response to decreased sulphate deposition, seven out of nine streams investigated had significantly decreasing sulphate concentrations (all trends were calculated with the Seasonal Kendall Test). The decrease in sulphate concentration was only minor, however, due to the release of previously stored soil sulphur. No increase was found in pH and acid neutralising capacity (defined by Reuss and Johnson, 1986). Aluminum concentrations in the streams did not decrease. Thus, no major acidification reversal can currently be noted in spite of two decades of decreased acid deposition. Nevertheless, the first signs of improvement in water quality were detected as there was a decrease in the level and frequency of extreme values of pH, acid neutralising capacity and aluminium concentrations in streams. With respect to nitrogen, no change was determined for either nitrate or ammonium concentrations in precipitation or stream water. Base cation fluxes indicate increasing net loss of base cations from all ecosystems investigated, which could be interpreted as an increase in soil acidification. The latter was due to a combination of continued high anion leaching and significant reduction of base cation deposition. No major improvement was noted in biological recovery, however, initial signs of recovery were detectable as there was re-occurrence of some single macroinvertebrate species which were formerly extinct. The results of this study have important implications for water authorities, forest managers and policy makers: the delay in acidification reversal suggests a need for ongoing intensive amelioration of waters, a careful selection of management tools to guarantee sustainable management of forests and the reduction of nitrogen deposition to prevent further acidification of soils and waters. Keywords: freshwater, acidification reversal, drinking water supply, forested catchments, Germany


2018 ◽  
Vol 27 ◽  
pp. 85-99 ◽  
Author(s):  
Martin Reiss ◽  
Peter Chifflard

Headwater springs in the German Low Mountain Ranges are local ecotone habitats and biogeographical islands embedded in and interlinked with their adjacent landscape. The structure of forests reflects the eco-hydrological conditions in substrate type occurrence, microhabitat richness and biodiversity in forest springs. This study considers effects from different forest land cover by comparing spring habitats in deciduous beech forests and coniferous spruce forests on eco-hydrological structures and biodiversity. Study areas include six different forest landscapes in the Low Mountain Ranges in Central Germany in Hesse and Thuringia. Hydro-morphological structure mapping and invertebrate sampling was executed within a multi-habitat sampling regime, which involves sampling plots being allocated according to the cover ratio of the occurring substrata. Aquatic and terrestrial spring zones are considered with respect to an ecotone approach. Some in situ measurements were implemented, such as pH values, to assess the acidity of the spring water. Results show obvious differences in acidity, substrate type cover ratios and biodiversity in deciduous and coniferous forest springs. Conifer forest springs were found tending to acidification while deciduous forest springs were slightly alkaline. Deciduous forest springs had higher cover ratios of organic microhabitats as well as a higher biodiversity in species richness and total number of individuals. Although it was not possible to clearly distinguish one direct key factor of fauna assemblages, negative effects from forest management practices (e.g. monoculture plantations of conifer forest) on spring habitats can be concluded.


Author(s):  
Charles Sheppard

Reefs in deep geological time have been built by a succession of different kinds of life: plant, bacterial, and animal. Stromatolites and bryozoans were major reef-builders that persist today in minor or non-reef-building forms, sponges built entire reefs and are still important reef components, while several groups of major reef-builders flourished for a while and then became extinct: archaeocyathids which were similar to sponges, and coral-like forms including rugose and tabulate corals. Today’s reef-builders, cnidarian corals, appeared well after the great Permian-Triassic extinction event. All of these groups deposited vast quantities of limestone rock on which they live, often visible today as low mountain ranges. Reefs grow to the surface but not beyond, but upon them sand and sediments may build up, forming an island that attracts plants, then birds and other terrestrial forms of life. The sediments become cemented with the aid of rainwater too, and ‘low islands’ develop. Many islands also show their old, central volcanoes, resulting in the vast array of different combinations of coral island type. Today, however, there is a coral reef crisis due to overexploitation of a reef’s rich resources, from pollution of several kinds, and climate change.


2020 ◽  
Author(s):  
Elody Fluck ◽  
Michael Kunz ◽  
Peter Geissbuehler ◽  
Stefan P. Ritz

Abstract. In this study we present a unique 10-year climatology of severe convective storm tracks for a larger European area covering Germany, France, Belgium and Luxembourg. For the period 2005–2014, a high-resolution hail potential composite of 1 by 1 km2 is produced from two-dimensional reflectivity radar data and lightning data. Individual hailstorm tracks as well as their physical properties, such as radar reflectivity along the tracks were reconstructed for the entire time period using the Convective Cell Tracking Algorithm (CCTA2D). A sea-to-continent gradient in the number of hail days is present over the whole domain. In addition, the highest number of severe storms is found on the leeward side of low mountain ranges such as near the Massif Central in France and the Swabian Jura in southwest Germany. A latitude shift in the hail peak month is observed between the northern part of Germany where hail occurs most frequently in August, and southern France where the maximum of hail occurs two months earlier. The spatially most extended footprints with high reflectivity values occurred on 9 June 2014 and on 28 July 2013 with lengths reaching several hundreds of kilometers. Both events implied hailstones measuring up to 10 cm which caused damage in excess of 2 Billions Euros.


1999 ◽  
Vol 61 (2-3) ◽  
pp. 193-200 ◽  
Author(s):  
R. Wassmuth ◽  
F. Wallbaum ◽  
H.-J. Langholz

2017 ◽  
Vol 85 (6) ◽  
Author(s):  
Christian Schwarz ◽  
Philipp Stöckle

In traditional dialectology, prominent geographical conditions are particularly made responsible for linguistic divergence between neighboring dialect areas (e. g. rivers, mountain ranges, etc.). Also modern national borders, territories of the Middle Ages or even older borders between tribal areas are made responsible as factors which consider linguistic areas as “mirror pictures of history” (Bach 1950: 31, translation: CS). Geographical as well as political borders seem to function as points of orientation that speakers use for constructing their cognitive surroundings and which consequently can result in linguistic divergence. In our contribution, we want to focus on the question of how the topographic nature of land-scapes influences the mental construction of linguistic areas by lay speakers. For pursuing this question, we will discuss results from German dialect areas that cover a broad range of different topographic landscape forms. The analyzed areas are located in the utter southwest of Germany (characterized by flat lands along the Rhine valley and low mountain ranges of the Black Forest) and in South Tyrol in the very north of Italy (characterized by mountains and deep valley cuttings). In our contribution, we will argue that speakers in their subjective dialect perception orient themselves toward national borders and topographically prominent points. With regard to topography primarily valleys are used as eponyms for subjective dialect areas.


Sign in / Sign up

Export Citation Format

Share Document