High resolution climatic monsoonal variability reconstructed from a continuous ~2700 year sediment record from Northwest Himalaya Ladakh / (Record no. 15039)
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fixed length control field | 02737nab a2200277 4500 |
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control field | 20231026115340.0 |
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fixed length control field | 231026b |||||||| |||| 00| 0 eng d |
100 ## - MAIN ENTRY--PERSONAL NAME | |
Personal name | Sharma, Choudhurimayum Pankaj |
245 ## - TITLE STATEMENT | |
Title | High resolution climatic monsoonal variability reconstructed from a continuous ~2700 year sediment record from Northwest Himalaya Ladakh / |
260 ## - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT) | |
Name of publisher, distributor, etc | Sage, |
Date of publication, distribution, etc | 2020. |
300 ## - PHYSICAL DESCRIPTION | |
Pages | Vol. 30, issue 3, 2020 ( 441–457 p.). |
520 ## - SUMMARY, ETC. | |
Summary, etc | A chronologically well-constrained sedimentary archive from Upshi (Ladakh) was studied using a multi-proxy approach namely palynology, environmental magnetism, total organic carbon (TOC), total nitrogen (TN), stable isotopes of carbon and nitrogen providing a continuous vegetation, and paleoenvironmental history spanning the last ~2700 years with a temporal resolution of ~43 years. Pollen assemblage shows non-arboreal pollen (NAP) and non-pollen palynomorph (NPP) were dominant around the Upshi from ~2646 to 2431 cal. yr BP, indicating warmer conditions. Arboreal pollen (AP) and NAP gradually increased from 2431 to 1860 cal. yr BP in the study area, under warm and wet conditions, corresponding to the Roman Warm Period (RWP). This phase also witnessed enhanced sediment δ15N and χlf values. From ~1860 to ~1154 cal. yr BP increased Chenopodiaceae/Amaranthaceae and substantial spread of NPP suggest decreased temperature and prevalence of cold-dry climate. This period also records declining trends of χlf, δ15N, δ13Corg, TOC, and TN contents. From ~1154 to 293 cal. yr BP, the vegetation type reversed to mixed conifer and broad-leaved forest with significant increase in herbaceous taxa, rising δ15N, δ13Corg, TOC, and TN suggesting warm and wet conditions in the study area. This period broadly corresponds to the ‘Medieval Warm Period’ (MWP). Among all the proxies employed, depth profiles of TOC and TN (wt%) appear to respond best against external climate forcing showing remarkable correlation(s) with residual Δ14C in atmosphere, indicating dominance of intrinsic solar variability on regional climate/environment. The reconstructed recorded is well connected with established historical events and cultural activities of the Eurasian region. |
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Added Entry Personal Name | Rawat, Suman Lata |
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Added Entry Personal Name | Srivastava, Pradeep |
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Added Entry Personal Name | Meena, Narendra K |
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Added Entry Personal Name | Agnihotri, Rajesh |
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Added Entry Personal Name | Kumar, Anil |
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Added Entry Personal Name | Chahal, Poonam |
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Added Entry Personal Name | Gahlaud, SKS |
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Added Entry Personal Name | Shukla, UK |
773 0# - HOST ITEM ENTRY | |
Host Biblionumber | 12756 |
Host Itemnumber | 17200 |
Place, publisher, and date of publication | London: Sage Publication Ltd, 2019. |
Title | Holocene/ |
International Standard Serial Number | 09596836 |
856 ## - ELECTRONIC LOCATION AND ACCESS | |
Uniform Resource Identifier | https://doi.org/10.1177/0959683619887426 |
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Koha item type | E-Journal |
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