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Supplemental material, sj-docx-2-hol-10.1177_09596836231163486 for Late-Holocene hydrological variability from the NW Himalaya and southwestern Tibetan Plateau: Paleo-salinity records from Pangong Tso by Sumit Sagwal, Anil Kumar, Choudhurimayum Pankaj Sharma, Pradeep Srivastava, Shravi Agarwal and Ravi Bhushan in The Holocene

Supplemental material, sj-docx-1-hol-10.1177_09596836231157066 for Late-Holocene wildfire record from the Stagmo peat section, Leh valley, NW Himalaya by Sumit Sagwal, Dipanwita Sengupta, Anil Kumar, Som Dutt, Pradeep Srivastava, Rajesh Agnihotri, Sanjay Kumar Singh Gahlaud, Partha Sarathi Jena, Ajay Shivam and Ravi Bhushan in The Holocene

Supplemental material, sj-docx-1-hol-10.1177_09596836231157066 for Late-Holocene wildfire record from the Stagmo peat section, Leh valley, NW Himalaya by Sumit Sagwal, Dipanwita Sengupta, Anil Kumar, Som Dutt, Pradeep Srivastava, Rajesh Agnihotri, Sanjay Kumar Singh Gahlaud, Partha Sarathi Jena, Ajay Shivam and Ravi Bhushan in The Holocene

Supplemental material, sj-docx-3-hol-10.1177_09596836231163486 for Late-Holocene hydrological variability from the NW Himalaya and southwestern Tibetan Plateau: Paleo-salinity records from Pangong Tso by Sumit Sagwal, Anil Kumar, Choudhurimayum Pankaj Sharma, Pradeep Srivastava, Shravi Agarwal and Ravi Bhushan in The Holocene

This research assesses the impacts of climate change and relative sea level (RSL) fluctuations on coastal vegetation during the past 2000 years along the Mahanadi River delta, Northeast coast of India. Sediment samples of a 2.6 m trench from Barhatubi area located in the lower flood plain of Mahanadi River delta were studied for sedimentological and pollen analysis. Mangrove succession can be divided into three zones: (1) Freshwater marsh (∼1980-1420 cal yr BP); (2) Tidal flat (∼1420-770 cal yr BP) and (3) Landward mangrove margin (∼770 cal yr BP-Present). A transgressive shift from floodplain freshwater marsh to a tidal flat is recorded between ∼1980-1420 cal yr BP which is evidenced by upland tree taxa, Poaceae, pteridophyte and fungal spores along with low percentage of mangroves such as Avicennia, Sonneratia and Rhizophora representing the landward edge of the tidal region. Dominance of Sonneratia and a decline in terrestrial taxa reflects a rise in the relative sea level around ∼1420 cal yr BP with less freshwater input from land suggesting a weakened monsoon condition. After ∼770 cal yr BP, an overall regressive phase with small cycles of relative sea level rise/fall has been observed due to the dominance of salt tolerant Avicennia along with Rhizophora, Excoecaria agallocha and Aegialitis rotundifolia alternating with Sonneratia and other marine palynomorphs.

Supplemental material, sj-docx-1-hol-10.1177_09596836231163486 for Late-Holocene hydrological variability from the NW Himalaya and southwestern Tibetan Plateau: Paleo-salinity records from Pangong Tso by Sumit Sagwal, Anil Kumar, Choudhurimayum Pankaj Sharma, Pradeep Srivastava, Shravi Agarwal and Ravi Bhushan in The Holocene

Supplemental material, sj-docx-2-hol-10.1177_09596836231163486 for Late-Holocene hydrological variability from the NW Himalaya and southwestern Tibetan Plateau: Paleo-salinity records from Pangong Tso by Sumit Sagwal, Anil Kumar, Choudhurimayum Pankaj Sharma, Pradeep Srivastava, Shravi Agarwal and Ravi Bhushan in The Holocene

Supplemental material, sj-docx-3-hol-10.1177_09596836231163486 for Late-Holocene hydrological variability from the NW Himalaya and southwestern Tibetan Plateau: Paleo-salinity records from Pangong Tso by Sumit Sagwal, Anil Kumar, Choudhurimayum Pankaj Sharma, Pradeep Srivastava, Shravi Agarwal and Ravi Bhushan in The Holocene

Supplemental material, Supplementary_figures for Early Holocene Indian summer monsoon and its impact on vegetation in the Central Himalaya: Insight from δD and δ13C values of leaf wax lipid by Sambit Ghosh, Prasanta Sanyal, Sohom Roy, Ravi Bhushan, SP Sati, Anne Philippe and Navin Juyal in The Holocene

In this article I develop a model that accounts for interdependence between trading costs in various asset markets arising from the optimizing behavior of liquidity traders. The model suggests that noise trading is an important determinant of the liquidity of asset markets and provides a positive theory for diversified asset holding by risk-neutral liquidity traders. Article published by Oxford University Press on behalf of the Society for Financial Studies in its journal, The Review of Financial Studies.