Modern pollen-vegetation-stable carbon isotope analogues of Bakhira lake, central Ganga plain, India: implications for palaeoclimatic and palaeoecological reconstruction

A multiproxy modern surface sediments sample analogue including pollen, non-pollen palynomorphs (NPPs), Total organic carbon/Total nitrogen (TOC/TN), and stable carbon isotopes (δ 13 C values) were generated from the Bakhira Lake, Central Ganga Plain (CGP) to delineate the modern climate-vegetation relationship and human-environment interactions. Pollen data reveal a dominance of non-arboreals (67.4%) over arboreals (32.6%) along the lake margins, with increased arboreal representation (e.g. Acacia , Madhuca indica , Anacardiaceae, Trewia nudiflora , Peltophorum , Arecaceae) in the lake centre. This reflects both land-use intensity and pollen production biases. The assemblage indicates a mixed deciduous forest under warm, humid conditions. The occurrence of marker pollen taxa, such as Cerealia, Alternanthera , Asteraceae, Chenopodiaceae/Amaranthaceae (Cheno/Am), Brassicaceae and NPPs along with coprophilous fungi assemblage (viz. Sordaria , Podospora, Delitschia , and Ascodesmis ) shows the anthropogenic activities and intensively-grazed conditions over the sampling site. The relatively higher δ 13 C values (−19.7 to −21.7‰) indicate C 3 dominated to mixed C 3 −C 4 vegetation input to the sedimentary organic matter at the lake centre. The NW and SE flanks, together with cropland, have relatively lower δ 13 C values ranging from −21.2‰ to −28.9‰, except for the sample number S23 (−19.3‰), indicating a higher contribution of organic matter from C 3 vegetation. Ordination analysis of pollen taxa distributions in surface sediments samples revealed correlations among sampling locations, modern pollen deposition, and associated environmental factors. This multiproxy modern dataset provides a robust baseline for interpreting Holocene palaeoecological and palaeoclimatic dynamics across tropical lacustrine systems in the central Indian subcontinent.

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Journal
The Holocene
Published
2026-06-26
DOI
https://doi.org/10.1177/09596836261458257
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00

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article

Modern pollen-vegetation-stable carbon isotope analogues of Bakhira lake, central Ganga plain, India: implications for palaeoclimatic and palaeoecological reconstruction

Anupam Sharma, Parminder Singh Ranhotra, Shailesh Agrawal, Anjali Trivedi et al.
The Holocene
Geology and Paleoclimatology Research
article

Modern pollen-vegetation-stable carbon isotope analogues of Bakhira lake, central Ganga plain, India: implications for palaeoclimatic and palaeoecological reconstruction

Anupam Sharma, Parminder Singh Ranhotra, Shailesh Agrawal, Anjali Trivedi, Mohd Ikram
article en

Abstract

A multiproxy modern surface sediments sample analogue including pollen, non-pollen palynomorphs (NPPs), Total organic carbon/Total nitrogen (TOC/TN), and stable carbon isotopes (δ 13 C values) were generated from the Bakhira Lake, Central Ganga Plain (CGP) to delineate the modern climate-vegetation relationship and human-environment interactions. Pollen data reveal a dominance of non-arboreals (67.4%) over arboreals (32.6%) along the lake margins, with increased arboreal representation (e.g. Acacia , Madhuca indica , Anacardiaceae, Trewia nudiflora , Peltophorum , Arecaceae) in the lake centre. This reflects both land-use intensity and pollen production biases. The assemblage indicates a mixed deciduous forest under warm, humid conditions. The occurrence of marker pollen taxa, such as Cerealia, Alternanthera , Asteraceae, Chenopodiaceae/Amaranthaceae (Cheno/Am), Brassicaceae and NPPs along with coprophilous fungi assemblage (viz. Sordaria , Podospora, Delitschia , and Ascodesmis ) shows the anthropogenic activities and intensively-grazed conditions over the sampling site. The relatively higher δ 13 C values (−19.7 to −21.7‰) indicate C 3 dominated to mixed C 3 −C 4 vegetation input to the sedimentary organic matter at the lake centre. The NW and SE flanks, together with cropland, have relatively lower δ 13 C values ranging from −21.2‰ to −28.9‰, except for the sample number S23 (−19.3‰), indicating a higher contribution of organic matter from C 3 vegetation. Ordination analysis of pollen taxa distributions in surface sediments samples revealed correlations among sampling locations, modern pollen deposition, and associated environmental factors. This multiproxy modern dataset provides a robust baseline for interpreting Holocene palaeoecological and palaeoclimatic dynamics across tropical lacustrine systems in the central Indian subcontinent.

The Holocene
Academy of Scientific and Innovative Research (IN)
Birbal Sahni Institute of Palaeosciences
Climate action
Openalex Percentile: Top 7%
Geology and Paleoclimatology Research
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