Please use this identifier to cite or link to this item: http://dx.doi.org/10.25673/93441
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dc.contributor.authorHöser, Norbertger
dc.date.accessioned2022-11-16T08:25:05Z-
dc.date.available2022-11-16T08:25:05Z-
dc.date.issued2012
dc.identifier.issn2195-531X
dc.identifier.otherBd. 45 Nr. 2 (2012): N.F. Hercynia
dc.identifier.urihttps://opendata.uni-halle.de//handle/1981185920/95397-
dc.identifier.urihttp://dx.doi.org/10.25673/93441-
dc.description.abstractHöser, N.: Earthworms (Oligochaeta: Lumbricidae) in a slope soil catena. - Hercynia N. F. 45 (2012): 193 –208 In studies of slope–valley floor soil profiles, the characteristic species spectrum of earthworms in Central German lime-hornbeam-oak woodland was determined. Dendrobaena vejdovskyi and D. pygmaea emerge as the character species. With the development of humus horizons in the soil profile, D. octaedra and Dendrodrilus rubidus appear. In the core areas of soils in wet locations, Eiseniella tetraedra, Aporrectodealimicola, and Murchieona muldali are found.It is characteristic of the relief sequence of the slope–valley floor profile that Proctodrilus antipai inhabits the edge of the valley bottom at the foot of the slope, while P. tuberculatus occurs both on the slope itself and in the alluvial meadows of the valley floor.On the slope and in the valley bottom soil, the layer profiles provide the abiotic preconditions for the ecological niches required by earthworms. This is discussed using the example of suspended capillary water at the layer boundaries, which is apparently a soil attribute attractive to P. tuberculatus and resting stages of Aporrectodea species. The relationships between endogeic and anecic species and soil displacement on slopes, in alluvial meadows, and in arable fields show that Ap. caliginosa and Octolasion cyaneum are associated with early developmental phases (or illuvial characteristics) of mineral soils, and that O. lacteum prefers soils closer to a climax profile with more humus. Since soil displacements, owing to the long formation times of new soil horizons, are erased only after a long period of time, while on the other hand intact horizons remain in the “memory” of a soil for just as long, the presence of Ap. caliginosa and O. cyaneum in woodland indicates past soil displacements, and presence of O. lacteum in areas without trees indicates that woodland was once present.eng
dc.language.isoeng
dc.publisherHercynia - Ökologie und Umwelt in Mitteleuropaeng
dc.relation.ispartofHercynia - Ökologie und Umwelt in Mitteleuropaeng
dc.rights.urihttps://creativecommons.org/licenses/by-nd/4.0/
dc.subject.ddc000
dc.titleRegenwürmer (Oligochaeta: Lumbricidae) in der Hangcatenager
dc.typeArticle
local.bibliographicCitation.journaltitleHercynia - Ökologie und Umwelt in Mitteleuropaeng
local.bibliographicCitation.volume45
local.bibliographicCitation.issue2
local.bibliographicCitation.pagestart193
local.bibliographicCitation.pageend193
local.openaccesstrue
dc.description.noteDie Hercynia publiziert Originalbeiträge mit dem Schwerpunkt Ökologie (mit ihren vielseitigen Aspekten der Biodiversität), Botanik, Zoologie, Geologie und Geografie, den anwendungsorientierten Bereichen des Natur- und Umweltschutzes, sowie der Land- und Forstwirtschaft.eng
local.bibliographicCitation.urihttps://public.bibliothek.uni-halle.de/hercynia/article/view/1733/version/1715
local.accessrights.dnbfree
dc.identifier.externalojs150
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