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Peloturbation (Churning, Hydroturbation, Self Mulching)
F. Bailly et al. (2000): Synsedimentäre Paläo-Vertisole im Oberjura des westlichen Wiehengebirges. PDF file (in German), Osnabrücker Naturwissenschaftliche Mitteilungen, 26: 15-46.
P. Driessen et al.: Lecture notes on the major soils of the world. Abstract.
Sabine Fiedler and Iris Palmer: Systematik von Böden. U.S. Soil Taxonomy (2003). PDF file, in German.
GeoDZ.com: Peloturbation, Pedoturbation and Selbstmulcheffekt (in German).
G.H. Mack et al. (1993):
Classification
of paleosols.
Abstract, GSA Bulletin, 105: 129–136.
See also
here.
Rolf Nieder and Dinesh K. Benbi (2008):
Carbon
and nitrogen in the terrestrial environment (Google books). Go to page 27:
!
"Soils that are repeatedly wetted and dried and that contain clays with a large capacity
for expansion tend to crack widely and deeply, allowing topsoil particles and organic materials to
fall into lower soil layers, so that over time the whole soil is turned over [...]. This process
is called peloturbation". See also fig. 1.15!
!
T.J. Orr and E.M. Roberts (2024):
A
review and field guide for the standardized description and sampling of paleosols. Open access,
Earth-Science Reviews, 253.
"... Paleosols are unrivaled terrestrial archives of paleoclimatic, paleoecological, and paleoenvironmental conditions
[...] we have illustrated and tabulated key paleosol features and classification schemes,
including horizon determination and classification; ped determination and classification;
mottle description; mineral accumulation description/morphology; burrow/chamber morphology
and description; and rhizolith morphology and classification ..."
! C. Owen et al. (2021): Recognising triggers for soft-sediment deformation: Current understanding and future directions. Sedimentary Geology, 235: 133–140. See also here.
R.R. Schoch and D. Seegis (2014): Taphonomy, deposition and pedogenesis in the Upper Triassic dinosaur beds of Trossingen. Abstract, Palaeobiodiversity and Palaeoenvironments, 94: 571–593. See also here (in PDF).
!
A.J. van Loon (2009):
Soft-sediment
deformation structures in siliciclastic sediments: an overview. I)n PDF,
Geologos, 15: 3–55.
See also
here.
"... various deformational processes, which are subdivided here into (1) endogenic
processes resulting in endoturbations; (2) gravity-dominated processes resulting in graviturbations, which can be
subdivided further into (2a) astroturbations, (2b) praecipiturbations, (2c) instabiloturbations, (2d) compagoturbations
and (2e) inclinaturbations; and (3) exogenic processes resulting in exoturbations, which can be further subdivided into
(3a) bioturbations – with subcategories (3a’) phytoturbations, (3a’’) zooturbations and (3a’’’) anthropoturbations – (3b)
glaciturbations, (3c) thermoturbations, (3d) hydroturbations, (3e) chemoturbations, and (3f)
eoloturbations. ..."
Wikipedia, the free encyclopedia:
!
Bioturbation.
!
Soil biomantle.
Soil Science.
World
Reference Base for Soil Resources.
Category:Soil science.
!
Hydroturbation,
auch Peloturbation genannt (in German).
Bioturbation.
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