Fluvial dynamics and 14 C‐ 10 Be disequilibrium on the Bolivian Altiplano
Determining sediment transfer times is key to understanding source-to-sink dynamics and the transmission of environmental signals through the fluvial system. Previous work on the Bolivian Altiplano applied the in situ cosmogenic 14 C- 10 Be-chronometer to river sands and proposed sediment storage ti...
Published in: | Earth Surface Processes and Landforms |
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2019
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Online Access: | https://pure.au.dk/portal/da/publications/fluvial-dynamics-and-14c10be-disequilibrium-on-the-bolivian-altiplano(3de15aad-e4a8-48a5-8f93-c6562e993d16).html https://doi.org/10.1002/esp.4529 http://www.scopus.com/inward/record.url?scp=85056777629&partnerID=8YFLogxK |
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ftuniaarhuspubl:oai:pure.atira.dk:publications/3de15aad-e4a8-48a5-8f93-c6562e993d16 2023-05-15T16:39:22+02:00 Fluvial dynamics and 14 C‐ 10 Be disequilibrium on the Bolivian Altiplano Hippe, Kristina Gordijn, Tiemen Hajdas, Irka Jansen, John Christl, Marcus Vockenhuber, Christof Maden, Colin Akcar, Naki Ivy-Ochs, Susan 2019 https://pure.au.dk/portal/da/publications/fluvial-dynamics-and-14c10be-disequilibrium-on-the-bolivian-altiplano(3de15aad-e4a8-48a5-8f93-c6562e993d16).html https://doi.org/10.1002/esp.4529 http://www.scopus.com/inward/record.url?scp=85056777629&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Hippe , K , Gordijn , T , Hajdas , I , Jansen , J , Christl , M , Vockenhuber , C , Maden , C , Akcar , N & Ivy-Ochs , S 2019 , ' Fluvial dynamics and 14 C‐ 10 Be disequilibrium on the Bolivian Altiplano ' , Earth Surface Processes and Landforms , vol. 44 , no. 3 , pp. 766-780 . https://doi.org/10.1002/esp.4529 C-14-Be-10 chronometer CENTRAL ANDES COSMOGENIC RADIONUCLIDES DEBRIS-FLOW DENUDATION RATES GLACIAL HISTORY HYDROLOGIC VARIATION ICE-CORE LAKE TITICACA LATE PLEISTOCENE SEDIMENT PRODUCTION cosmogenic nuclide dating radiocarbon dating sediment steady-state storage article 2019 ftuniaarhuspubl https://doi.org/10.1002/esp.4529 2022-12-28T23:55:11Z Determining sediment transfer times is key to understanding source-to-sink dynamics and the transmission of environmental signals through the fluvial system. Previous work on the Bolivian Altiplano applied the in situ cosmogenic 14 C- 10 Be-chronometer to river sands and proposed sediment storage times of ~10–20 kyr in four catchments southeast of Lake Titicaca. However, the fidelity of those results hinges upon isotopic steady-state within sediment supplied from the source area. With the aim of independently quantifying sediment storage times and testing the 14 C- 10 Be steady-state assumption, we dated sediment storage units within one of the previously investigated catchments using radiocarbon dating, cosmogenic 10 Be- 26 Al isochron burial dating, and 10 Be- 26 Al depth-profile dating. Palaeosurfaces appear to preserve remnants of a former fluvial system, which has undergone drainage reversal, reduction in catchment area, and local isostatic uplift since ~2.8 Ma. From alluvium mantling the palaeosurfaces we gained a deposition age of ~580 ka, while lower down fluvial terraces yielded ≤34 ka, and floodplains ~3–1 ka. Owing to restricted channel connectivity with the terraces and palaeosurfaces, the main source of channel sediment is via reworking of the late Holocene floodplain. Yet modelling a set of feasible scenarios reveals that floodplain storage and burial depth are incompatible with the 14 C- 10 Be disequilibrium measured in the channel. Instead we propose that the 14 C- 10 Be offset results from: (i) non-uniform erosion whereby deep gullies supply hillslope-derived debris; and/or (ii) holocene landscape transience associated with climate or human impact. The reliability of the 14 C- 10 Be chronometer vitally depends upon careful evaluation of sources of isotopic disequilibrium in a wide range of depositional and erosional landforms in the landscape. Article in Journal/Newspaper ice core Aarhus University: Research Earth Surface Processes and Landforms 44 3 766 780 |
institution |
Open Polar |
collection |
Aarhus University: Research |
op_collection_id |
ftuniaarhuspubl |
language |
English |
topic |
C-14-Be-10 chronometer CENTRAL ANDES COSMOGENIC RADIONUCLIDES DEBRIS-FLOW DENUDATION RATES GLACIAL HISTORY HYDROLOGIC VARIATION ICE-CORE LAKE TITICACA LATE PLEISTOCENE SEDIMENT PRODUCTION cosmogenic nuclide dating radiocarbon dating sediment steady-state storage |
spellingShingle |
C-14-Be-10 chronometer CENTRAL ANDES COSMOGENIC RADIONUCLIDES DEBRIS-FLOW DENUDATION RATES GLACIAL HISTORY HYDROLOGIC VARIATION ICE-CORE LAKE TITICACA LATE PLEISTOCENE SEDIMENT PRODUCTION cosmogenic nuclide dating radiocarbon dating sediment steady-state storage Hippe, Kristina Gordijn, Tiemen Hajdas, Irka Jansen, John Christl, Marcus Vockenhuber, Christof Maden, Colin Akcar, Naki Ivy-Ochs, Susan Fluvial dynamics and 14 C‐ 10 Be disequilibrium on the Bolivian Altiplano |
topic_facet |
C-14-Be-10 chronometer CENTRAL ANDES COSMOGENIC RADIONUCLIDES DEBRIS-FLOW DENUDATION RATES GLACIAL HISTORY HYDROLOGIC VARIATION ICE-CORE LAKE TITICACA LATE PLEISTOCENE SEDIMENT PRODUCTION cosmogenic nuclide dating radiocarbon dating sediment steady-state storage |
description |
Determining sediment transfer times is key to understanding source-to-sink dynamics and the transmission of environmental signals through the fluvial system. Previous work on the Bolivian Altiplano applied the in situ cosmogenic 14 C- 10 Be-chronometer to river sands and proposed sediment storage times of ~10–20 kyr in four catchments southeast of Lake Titicaca. However, the fidelity of those results hinges upon isotopic steady-state within sediment supplied from the source area. With the aim of independently quantifying sediment storage times and testing the 14 C- 10 Be steady-state assumption, we dated sediment storage units within one of the previously investigated catchments using radiocarbon dating, cosmogenic 10 Be- 26 Al isochron burial dating, and 10 Be- 26 Al depth-profile dating. Palaeosurfaces appear to preserve remnants of a former fluvial system, which has undergone drainage reversal, reduction in catchment area, and local isostatic uplift since ~2.8 Ma. From alluvium mantling the palaeosurfaces we gained a deposition age of ~580 ka, while lower down fluvial terraces yielded ≤34 ka, and floodplains ~3–1 ka. Owing to restricted channel connectivity with the terraces and palaeosurfaces, the main source of channel sediment is via reworking of the late Holocene floodplain. Yet modelling a set of feasible scenarios reveals that floodplain storage and burial depth are incompatible with the 14 C- 10 Be disequilibrium measured in the channel. Instead we propose that the 14 C- 10 Be offset results from: (i) non-uniform erosion whereby deep gullies supply hillslope-derived debris; and/or (ii) holocene landscape transience associated with climate or human impact. The reliability of the 14 C- 10 Be chronometer vitally depends upon careful evaluation of sources of isotopic disequilibrium in a wide range of depositional and erosional landforms in the landscape. |
format |
Article in Journal/Newspaper |
author |
Hippe, Kristina Gordijn, Tiemen Hajdas, Irka Jansen, John Christl, Marcus Vockenhuber, Christof Maden, Colin Akcar, Naki Ivy-Ochs, Susan |
author_facet |
Hippe, Kristina Gordijn, Tiemen Hajdas, Irka Jansen, John Christl, Marcus Vockenhuber, Christof Maden, Colin Akcar, Naki Ivy-Ochs, Susan |
author_sort |
Hippe, Kristina |
title |
Fluvial dynamics and 14 C‐ 10 Be disequilibrium on the Bolivian Altiplano |
title_short |
Fluvial dynamics and 14 C‐ 10 Be disequilibrium on the Bolivian Altiplano |
title_full |
Fluvial dynamics and 14 C‐ 10 Be disequilibrium on the Bolivian Altiplano |
title_fullStr |
Fluvial dynamics and 14 C‐ 10 Be disequilibrium on the Bolivian Altiplano |
title_full_unstemmed |
Fluvial dynamics and 14 C‐ 10 Be disequilibrium on the Bolivian Altiplano |
title_sort |
fluvial dynamics and 14 c‐ 10 be disequilibrium on the bolivian altiplano |
publishDate |
2019 |
url |
https://pure.au.dk/portal/da/publications/fluvial-dynamics-and-14c10be-disequilibrium-on-the-bolivian-altiplano(3de15aad-e4a8-48a5-8f93-c6562e993d16).html https://doi.org/10.1002/esp.4529 http://www.scopus.com/inward/record.url?scp=85056777629&partnerID=8YFLogxK |
genre |
ice core |
genre_facet |
ice core |
op_source |
Hippe , K , Gordijn , T , Hajdas , I , Jansen , J , Christl , M , Vockenhuber , C , Maden , C , Akcar , N & Ivy-Ochs , S 2019 , ' Fluvial dynamics and 14 C‐ 10 Be disequilibrium on the Bolivian Altiplano ' , Earth Surface Processes and Landforms , vol. 44 , no. 3 , pp. 766-780 . https://doi.org/10.1002/esp.4529 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1002/esp.4529 |
container_title |
Earth Surface Processes and Landforms |
container_volume |
44 |
container_issue |
3 |
container_start_page |
766 |
op_container_end_page |
780 |
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1766029718020161536 |