Universität zu Köln

Francke, Alexander ORCID: 0000-0002-0370-5802, Dosseto, Anthony, Panagiotopoulos, Konstantinos ORCID: 0000-0002-3158-7962, Leicher, Niklas ORCID: 0000-0002-3367-5982, Lacey, Jack H. ORCID: 0000-0002-6329-2149, Kyrikou, Styliani, Wagner, Bernd ORCID: 0000-0002-1369-7893, Zanchetta, Giovanni, Kouli, Katerina ORCID: 0000-0003-1656-1091 and Leng, Melanie J. (2019). Sediment residence time reveals Holocene shift from climatic to vegetation control on catchment erosion in the Balkans. Glob. Planet. Change, 177. S. 186 - 201. AMSTERDAM: ELSEVIER SCIENCE BV. ISSN 1872-6364

Full text not available from this repository.

Abstract

Understanding the evolution of soil systems on geological time scales has become fundamentally important to predict future landscape development in light of rapid global warming and intensifying anthropogenic impact. Here, we use an innovative uranium isotope-based technique combined with organic carbon isotopes and elemental ratios of sediments from Lake Ohrid (North Macedonia/Albania) to reconstruct soil system evolution in the lake's catchment during the last similar to 16,000 cal yr BP. Uranium isotopes are used to estimated the paleosediment residence time, defined as the time elapsed between formation of silt and clay sized detrital matter and final deposition. The chronology is based on new cryptotephra layers identified in the sediment sequence. The isotope and elemental data are compared to sedimentary properties and pollen from the same sample material to provide a better understanding of past catchment erosion and landscape evolution in the light of climate forcing, vegetation development, and anthropogenic land use. During the Late Glacial and the Early Holocene, when wide parts of the catchment were covered by open vegetation, wetter climates promoted the mobilisation of detrital matter with a short paleo-sediment residence time. This is explained by erosion of deeper parts of the weathering horizon from thin soils. Detrital matter with a longer paleo-sediment residence time, illustrating shallow erosion of thicker soils is deposited in drier climates. The coupling between climatic variations and soil erosion terminates at the Early to Mid-Holocene transition as evidenced by a pronounced shift in uranium isotope ratios indicating that catchment erosion is dominated by shallow erosion of thick soils only. This shift suggests a threshold is crossed in hillslope erosion, possibly as a result of a major change in vegetation cover preventing deep erosion of thin soils at higher elevation. The threshold in catchment erosion is not mirrored by soil development over time, which gradually increases in response to Late Glacial to Holocene warming until human land use during the Late Holocene promotes reduced soil development and soil degradation. Overall, we observe that soil system evolution is progressively controlled by climatic, vegetation, and eventually by human land use over the last similar to 16,000 years.

Item Type:	Journal Article
Creators:	Creators Email ORCID ORCID Put Code Francke, Alexander UNSPECIFIED orcid.org/0000-0002-0370-5802 UNSPECIFIED Dosseto, Anthony UNSPECIFIED UNSPECIFIED UNSPECIFIED Panagiotopoulos, Konstantinos UNSPECIFIED orcid.org/0000-0002-3158-7962 UNSPECIFIED Leicher, Niklas UNSPECIFIED orcid.org/0000-0002-3367-5982 UNSPECIFIED Lacey, Jack H. UNSPECIFIED orcid.org/0000-0002-6329-2149 UNSPECIFIED Kyrikou, Styliani UNSPECIFIED UNSPECIFIED UNSPECIFIED Wagner, Bernd UNSPECIFIED orcid.org/0000-0002-1369-7893 UNSPECIFIED Zanchetta, Giovanni UNSPECIFIED UNSPECIFIED UNSPECIFIED Kouli, Katerina UNSPECIFIED orcid.org/0000-0003-1656-1091 UNSPECIFIED Leng, Melanie J. UNSPECIFIED UNSPECIFIED UNSPECIFIED
URN:	urn:nbn:de:hbz:38-147236
DOI:	10.1016/j.gloplacha.2019.04.005
Journal or Publication Title:	Glob. Planet. Change
Volume:	177
Page Range:	S. 186 - 201
Date:	2019
Publisher:	ELSEVIER SCIENCE BV
Place of Publication:	AMSTERDAM
ISSN:	1872-6364
Language:	English
Faculty:	Faculty of Mathematics and Natural Sciences
Divisions:	Faculty of Mathematics and Natural Sciences > Department of Geosciences > Institute of Geology and Mineralog
Subjects:	no entry
Uncontrolled Keywords:	Keywords Language URANIUM-SERIES ISOTOPES; LAKE OHRID MACEDONIA; LAND-USE; ENVIRONMENTAL-CHANGE; TEPHROSTRATIGRAPHIC RECORD; WEATHERING PROFILES; GALICICA MOUNTAINS; 637 KA; ALBANIA; PRESPA Multiple languages Geography, Physical; Geosciences, Multidisciplinary Multiple languages
Refereed:	Yes
URI:	http://kups.ub.uni-koeln.de/id/eprint/14723