Late-Holocene climatic record from a glacial lake in Ladakh range, Trans-Himalaya, India

A multi-proxy study using mineral magnetism, sediment texture, total organic content, palynofacies and diatoms was conducted in one of the highest proglacial lake situated at North Pulu (5098 m a.s.l.) of Ladakh sector of NW Himalaya – a high-altitude cold arid desert. This study presents climatic v...

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Published inHolocene (Sevenoaks) Vol. 30; no. 7; pp. 1029 - 1042
Main Authors Phartiyal, Binita, Singh, Randheer, Joshi, Priyanka, Nag, Debarati
Format Journal Article
LanguageEnglish
Published London, England SAGE Publications 01.07.2020
Sage Publications Ltd
Subjects
Anoxia
Anoxic conditions
Anoxic sediments
Aridity
Brittleness
Climate
Climate studies
Climate variability
Climatic conditions
Cold
Diatoms
Geochronology
Glacial lakes
Glaciers
High altitude
Holocene
Magnetism
Marine microorganisms
Meltwater
Nutrients
Palaeolimnology
Phase transitions
Sediment
Sediment texture
Sedimentation
Total organic carbon
Water levels
Tibetan Plateau
Ladakh
multi-proxy
proglacial lake
palaeoclimate
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Abstract A multi-proxy study using mineral magnetism, sediment texture, total organic content, palynofacies and diatoms was conducted in one of the highest proglacial lake situated at North Pulu (5098 m a.s.l.) of Ladakh sector of NW Himalaya – a high-altitude cold arid desert. This study presents climatic variations that occurred between 5412 and 419 cal. yr BP (14C AMS chronology). Directly recharged by meltwater from Khardung glacier, this proglacial lake provides a complete record of past climatic variability due to continuous sedimentation and this attribute makes it an exceptionally important geochronological archive for climatic studies. This first high-resolution palaeolimnology record from Karakoram Himalayas shows intermittent warm and cold periods in which the cold events are short but sudden events recorded at 5700, 4600, 4400, 4200, 3800, 3500, 3000, 1800–1700, 1200, 910, 840 and 770–710 cal. yr BP. Between 5412 and 4840 cal. yr BP, an oxic lake condition existed with freeze–thaw action, prominent weathering, more sediment generation and less organic productivity. The following period till 4410 cal. yr BP was cold and dry, a transition phase to the next warmer phase. Between 4410 and 2064 cal. yr BP, climate ameliorated to somewhat moderate warm climate and relatively high lake levels. Glacial melting due to a warm climate resulted in high TOC%, and well-preserved OM indicating reducing conditions in the lake system. From 2064 to 1711 cal. yr BP cold conditions and from 1272 to 1182 cal. yr BP warmer conditions are seen with large appearance in Amphora ovalis indicating increased nutrients input and moderate water levels. This was followed by warmer climatic conditions between 1182 and 958 cal. yr BP. LIA in the region is experienced between 958 and 644 cal. yr BP with anoxic condition. Between 644 and 419 cal. yr BP, climatic condition was again warmer comparatively. However, this warming was not so severe and only had a regional impact.
AbstractList A multi-proxy study using mineral magnetism, sediment texture, total organic content, palynofacies and diatoms was conducted in one of the highest proglacial lake situated at North Pulu (5098 m a.s.l.) of Ladakh sector of NW Himalaya – a high-altitude cold arid desert. This study presents climatic variations that occurred between 5412 and 419 cal. yr BP ( 14 C AMS chronology). Directly recharged by meltwater from Khardung glacier, this proglacial lake provides a complete record of past climatic variability due to continuous sedimentation and this attribute makes it an exceptionally important geochronological archive for climatic studies. This first high-resolution palaeolimnology record from Karakoram Himalayas shows intermittent warm and cold periods in which the cold events are short but sudden events recorded at 5700, 4600, 4400, 4200, 3800, 3500, 3000, 1800–1700, 1200, 910, 840 and 770–710 cal. yr BP. Between 5412 and 4840 cal. yr BP, an oxic lake condition existed with freeze–thaw action, prominent weathering, more sediment generation and less organic productivity. The following period till 4410 cal. yr BP was cold and dry, a transition phase to the next warmer phase. Between 4410 and 2064 cal. yr BP, climate ameliorated to somewhat moderate warm climate and relatively high lake levels. Glacial melting due to a warm climate resulted in high TOC%, and well-preserved OM indicating reducing conditions in the lake system. From 2064 to 1711 cal. yr BP cold conditions and from 1272 to 1182 cal. yr BP warmer conditions are seen with large appearance in Amphora ovalis indicating increased nutrients input and moderate water levels. This was followed by warmer climatic conditions between 1182 and 958 cal. yr BP. LIA in the region is experienced between 958 and 644 cal. yr BP with anoxic condition. Between 644 and 419 cal. yr BP, climatic condition was again warmer comparatively. However, this warming was not so severe and only had a regional impact.
A multi-proxy study using mineral magnetism, sediment texture, total organic content, palynofacies and diatoms was conducted in one of the highest proglacial lake situated at North Pulu (5098 m a.s.l.) of Ladakh sector of NW Himalaya – a high-altitude cold arid desert. This study presents climatic variations that occurred between 5412 and 419 cal. yr BP (14C AMS chronology). Directly recharged by meltwater from Khardung glacier, this proglacial lake provides a complete record of past climatic variability due to continuous sedimentation and this attribute makes it an exceptionally important geochronological archive for climatic studies. This first high-resolution palaeolimnology record from Karakoram Himalayas shows intermittent warm and cold periods in which the cold events are short but sudden events recorded at 5700, 4600, 4400, 4200, 3800, 3500, 3000, 1800–1700, 1200, 910, 840 and 770–710 cal. yr BP. Between 5412 and 4840 cal. yr BP, an oxic lake condition existed with freeze–thaw action, prominent weathering, more sediment generation and less organic productivity. The following period till 4410 cal. yr BP was cold and dry, a transition phase to the next warmer phase. Between 4410 and 2064 cal. yr BP, climate ameliorated to somewhat moderate warm climate and relatively high lake levels. Glacial melting due to a warm climate resulted in high TOC%, and well-preserved OM indicating reducing conditions in the lake system. From 2064 to 1711 cal. yr BP cold conditions and from 1272 to 1182 cal. yr BP warmer conditions are seen with large appearance in Amphora ovalis indicating increased nutrients input and moderate water levels. This was followed by warmer climatic conditions between 1182 and 958 cal. yr BP. LIA in the region is experienced between 958 and 644 cal. yr BP with anoxic condition. Between 644 and 419 cal. yr BP, climatic condition was again warmer comparatively. However, this warming was not so severe and only had a regional impact.
Author Joshi, Priyanka
Phartiyal, Binita
Nag, Debarati
Singh, Randheer
Author_xml – sequence: 1
  givenname: Binita
  orcidid: 0000-0003-3086-8735
  surname: Phartiyal
  fullname: Phartiyal, Binita
  email: binitaphartiyal@gmail.com
  organization: Birbal Sahni Institute of Palaeosciences, India
– sequence: 2
  givenname: Randheer
  surname: Singh
  fullname: Singh, Randheer
  organization: Birbal Sahni Institute of Palaeosciences, India
– sequence: 3
  givenname: Priyanka
  surname: Joshi
  fullname: Joshi, Priyanka
  organization: Birbal Sahni Institute of Palaeosciences, India
– sequence: 4
  givenname: Debarati
  surname: Nag
  fullname: Nag, Debarati
  organization: Birbal Sahni Institute of Palaeosciences, India
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multi-proxy
proglacial lake
palaeoclimate
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SSID ssj0016861
Score 2.4652307
Snippet A multi-proxy study using mineral magnetism, sediment texture, total organic content, palynofacies and diatoms was conducted in one of the highest proglacial...
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StartPage 1029
SubjectTerms Anoxia
Anoxic conditions
Anoxic sediments
Aridity
Brittleness
Climate
Climate studies
Climate variability
Climatic conditions
Cold
Diatoms
Geochronology
Glacial lakes
Glaciers
High altitude
Holocene
Magnetism
Marine microorganisms
Meltwater
Nutrients
Palaeolimnology
Phase transitions
Sediment
Sediment texture
Sedimentation
Total organic carbon
Water levels
Title Late-Holocene climatic record from a glacial lake in Ladakh range, Trans-Himalaya, India
URI https://journals.sagepub.com/doi/full/10.1177/0959683620908660
https://www.proquest.com/docview/2429455510
Volume 30
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