Geochemistry of Lake Heihai on the Tibetan Plateau
Reading the sediment record in terms of past climates is challenging since linking climate change to the associated responses of sedimentary systems is not always straightforward. Here we analyze the erosional response of landscapes on the Tibetan Plateau to interglacial climate forcing. Using the t...
Main Authors: | , , , , |
---|---|
Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2018
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.896505 https://doi.org/10.1594/PANGAEA.896505 |
id |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.896505 |
---|---|
record_format |
openpolar |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.896505 2023-05-15T15:09:06+02:00 Geochemistry of Lake Heihai on the Tibetan Plateau Ramisch, Arne Tjallingii, Rik Hartmann, Kai Diekmann, Bernhard Brauer, Achim MEDIAN LATITUDE: 35.991740 * MEDIAN LONGITUDE: 93.255775 * SOUTH-BOUND LATITUDE: 35.990000 * WEST-BOUND LONGITUDE: 93.251550 * NORTH-BOUND LATITUDE: 35.993480 * EAST-BOUND LONGITUDE: 93.260000 * DATE/TIME START: 2011-08-30T12:00:00 * DATE/TIME END: 2011-08-31T12:00:00 2018-12-04 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.896505 https://doi.org/10.1594/PANGAEA.896505 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.896505 https://doi.org/10.1594/PANGAEA.896505 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Ramisch, Arne; Tjallingii, Rik; Hartmann, Kai; Diekmann, Bernhard; Brauer, Achim (2018): Echo of the Younger Dryas in Holocene lake sediments on the Tibetan Plateau. Geophysical Research Letters, 45(20), 11154-11163, https://doi.org/10.1029/2018GL080225 AWI_Envi AWI_PerDyn AWI Arctic Land Expedition China2011,China2012/1,China2012/2,China2012/3 CN-Land_2012 Lake Heihai Qinghai China PC Permafrost Research (Periglacial Dynamics) @ AWI PG2057-1 Piston corer Polar Terrestrial Environmental Systems @ AWI Dataset 2018 ftpangaea https://doi.org/10.1594/PANGAEA.896505 https://doi.org/10.1029/2018GL080225 2023-01-20T07:34:16Z Reading the sediment record in terms of past climates is challenging since linking climate change to the associated responses of sedimentary systems is not always straightforward. Here we analyze the erosional response of landscapes on the Tibetan Plateau to interglacial climate forcing. Using the theory of dynamical systems on Holocene time series of geochemical proxies, we derive a sedimentary response model that accurately simulates observed proxy variation in three lake records. The model suggests that millennial variations in sediment composition reflect a self‐organization of landscapes in response to abrupt climate change between 11.6 and 11.9 ka BP. The self‐organization is characterized by oscillations in sediment supply emerging from a feedback between physical and chemical erosion processes, with estimated response times between 3,000 to 18,000 years depending on catchment topography. The implications of our findings emphasize the need for landscape response models to decipher the paleoclimatic code in continental sediment records. Dataset Arctic Climate change permafrost PANGAEA - Data Publisher for Earth & Environmental Science Arctic ENVELOPE(93.251550,93.260000,35.993480,35.990000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AWI_Envi AWI_PerDyn AWI Arctic Land Expedition China2011,China2012/1,China2012/2,China2012/3 CN-Land_2012 Lake Heihai Qinghai China PC Permafrost Research (Periglacial Dynamics) @ AWI PG2057-1 Piston corer Polar Terrestrial Environmental Systems @ AWI |
spellingShingle |
AWI_Envi AWI_PerDyn AWI Arctic Land Expedition China2011,China2012/1,China2012/2,China2012/3 CN-Land_2012 Lake Heihai Qinghai China PC Permafrost Research (Periglacial Dynamics) @ AWI PG2057-1 Piston corer Polar Terrestrial Environmental Systems @ AWI Ramisch, Arne Tjallingii, Rik Hartmann, Kai Diekmann, Bernhard Brauer, Achim Geochemistry of Lake Heihai on the Tibetan Plateau |
topic_facet |
AWI_Envi AWI_PerDyn AWI Arctic Land Expedition China2011,China2012/1,China2012/2,China2012/3 CN-Land_2012 Lake Heihai Qinghai China PC Permafrost Research (Periglacial Dynamics) @ AWI PG2057-1 Piston corer Polar Terrestrial Environmental Systems @ AWI |
description |
Reading the sediment record in terms of past climates is challenging since linking climate change to the associated responses of sedimentary systems is not always straightforward. Here we analyze the erosional response of landscapes on the Tibetan Plateau to interglacial climate forcing. Using the theory of dynamical systems on Holocene time series of geochemical proxies, we derive a sedimentary response model that accurately simulates observed proxy variation in three lake records. The model suggests that millennial variations in sediment composition reflect a self‐organization of landscapes in response to abrupt climate change between 11.6 and 11.9 ka BP. The self‐organization is characterized by oscillations in sediment supply emerging from a feedback between physical and chemical erosion processes, with estimated response times between 3,000 to 18,000 years depending on catchment topography. The implications of our findings emphasize the need for landscape response models to decipher the paleoclimatic code in continental sediment records. |
format |
Dataset |
author |
Ramisch, Arne Tjallingii, Rik Hartmann, Kai Diekmann, Bernhard Brauer, Achim |
author_facet |
Ramisch, Arne Tjallingii, Rik Hartmann, Kai Diekmann, Bernhard Brauer, Achim |
author_sort |
Ramisch, Arne |
title |
Geochemistry of Lake Heihai on the Tibetan Plateau |
title_short |
Geochemistry of Lake Heihai on the Tibetan Plateau |
title_full |
Geochemistry of Lake Heihai on the Tibetan Plateau |
title_fullStr |
Geochemistry of Lake Heihai on the Tibetan Plateau |
title_full_unstemmed |
Geochemistry of Lake Heihai on the Tibetan Plateau |
title_sort |
geochemistry of lake heihai on the tibetan plateau |
publisher |
PANGAEA |
publishDate |
2018 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.896505 https://doi.org/10.1594/PANGAEA.896505 |
op_coverage |
MEDIAN LATITUDE: 35.991740 * MEDIAN LONGITUDE: 93.255775 * SOUTH-BOUND LATITUDE: 35.990000 * WEST-BOUND LONGITUDE: 93.251550 * NORTH-BOUND LATITUDE: 35.993480 * EAST-BOUND LONGITUDE: 93.260000 * DATE/TIME START: 2011-08-30T12:00:00 * DATE/TIME END: 2011-08-31T12:00:00 |
long_lat |
ENVELOPE(93.251550,93.260000,35.993480,35.990000) |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change permafrost |
genre_facet |
Arctic Climate change permafrost |
op_source |
Supplement to: Ramisch, Arne; Tjallingii, Rik; Hartmann, Kai; Diekmann, Bernhard; Brauer, Achim (2018): Echo of the Younger Dryas in Holocene lake sediments on the Tibetan Plateau. Geophysical Research Letters, 45(20), 11154-11163, https://doi.org/10.1029/2018GL080225 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.896505 https://doi.org/10.1594/PANGAEA.896505 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.896505 https://doi.org/10.1029/2018GL080225 |
_version_ |
1766340333252116480 |