Revisiting afro-alpine Lake Garba Guracha in the Bale Mountains of Ethiopia: rationale, chronology, geochemistry, and paleoenvironmental implications

Bittner, L.; Bliedtner, M.; Grady, D.; Gil-Romera, G.; Martin-Jones, C.; Lemma, B.; Mekonnen, B.; Lamb, H. F.; Yang, H.; Glaser, B.; Szidat, S.; Salazar, G.; Rose, N. L.; Opgenoorth, L.; Miehe, G.; Zech, W.; Zech, M. (2020). Revisiting afro-alpine Lake Garba Guracha in the Bale Mountains of Ethiopia: rationale, chronology, geochemistry, and paleoenvironmental implications. Journal of paleolimnology, 64(3), pp. 293-314. Springer Nature 10.1007/s10933-020-00138-w

[img]
Preview
Text
Bittner_Sediment from Lake Garba Guracha in Bale Mountains (J Paleolim 2020).pdf - Published Version
Available under License Creative Commons: Attribution (CC-BY).
This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder.

Download (2MB) | Preview

Previous paleolimnological studies demonstrated that the sediments of Garba Guracha, situated at 3950 m asl in the afro-alpine zone of the Bale Mountains of Ethiopia, provide a complete Late Glacial and Holocene paleoclimate and environmental archive. We revisited Garba Guracha in order to retrieve new sediment cores and to apply new environmental proxies, e.g. charcoal, diatoms, biomarkers, and stable isotopes. Our chronology is established using 210Pb dating and radiocarbon dating of bulk sedimentary organic matter, bulk n-alkanes, and charcoal. Although bedrock was not reached during coring, basal ages confirm that sedimentation started at the earliest * 16 cal kyr BP. The absence of a systematic age offset for the n-alkanes suggests that ‘‘pre-aging’’ is not a prominent issue in this lake, which is characterised by a very small afro-alpine catchment. X-ray fluorescence scans and total organic carbon contents show a prominent transition from minerogenic to organic-rich sediments around 11 cal kyr BP coinciding with the Holocene onset. While an unambiguous terrestrial versus aquatic source identification seems challenging, the n-alkane-based Paq proxy, TOC/N ratios, d13C values, and the sugar biomarker patterns suggest a predominantly autochthonous organic matter source. Supraregional climate events, such as the African Humid Period, the Younger Dryas (YD), a 6.5 cal kyr BP short drying event, and the 4.2 cal kyr BP transition to overall drier climate are recorded in our archive. The Garba Guracha record suggests that northern hemisphere forcings played a role in the Eastern African highland paleoclimate.

Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Department of Chemistry, Biochemistry and Pharmaceutical Sciences (DCBP)
10 Strategic Research Centers > Oeschger Centre for Climate Change Research (OCCR)

UniBE Contributor:

Szidat, Sönke and Salazar Quintero, Gary Abdiel

Subjects:

500 Science > 570 Life sciences; biology
500 Science > 540 Chemistry

ISSN:

0921-2728

Publisher:

Springer Nature

Language:

English

Submitter:

Sönke Szidat

Date Deposited:

18 Nov 2020 12:04

Last Modified:

11 Mar 2021 10:12

Publisher DOI:

10.1007/s10933-020-00138-w

BORIS DOI:

10.7892/boris.147922

URI:

https://boris.unibe.ch/id/eprint/147922

Actions (login required)

Edit item Edit item
Provide Feedback