Binita Phartiyal

Dados Biográficos

ID	4454963
NOME	Binita Phartiyal
PRENOMES	Binita
SOBRENOME	Phartiyal
ASSINATURA	PHARTIYAL B
AFILIAÇÕES	Birbal Sahni Institute of Palaeosciences
ORCID	0000-0003-3086-8735
VERIFICADO	Sim
TOTAL DE OBRAS	18
TOTAL DE CITAÇÕES	6
TOTAL COMO AUTOR	18
TOTAL COMO EDITOR	0
PRIMEIRO ANO DE PUBLICAÇÃO	2007
ANO MAIS RECENTE DE PUBLICAÇÃO	2026
ÍNDICE H	2

Provenance and depositional processes of Plio-Pleistocene Karewa group sediments of Kashmir valley
Open AccessShirish Verma, Binita Phartiyal et al.ARTICLEQuaternary International2026Referências: 38
Climate-driven history of last 2600 years
Open AccessBinita Phartiyal, Balasubramanian Karthick et al.ARTICLEThe Holocene2025Referências: 88
A detailed reconstruction of Late-Holocene environmental and climatic dynamics has been achieved through systematic investigations conducted at Bandhavgarh National Park and Tiger Reserve in the Umaria district of Madhya Pradesh, Central India. Proxies such as mineral magnetism, textural analysis, carbon/nitrogen ratios, diatoms and pollen have been utilized in this research to elucidate the profound influence of climate on the region’s history a…
Late Quaternary fluvio-aeolian interactions and possible aridification in west-central India
Open AccessSourav Mukhopadhyay, Pratik Pandey et al.ARTICLEQuaternary International2025Referências: 3
Characterization of biotic and abiotic signatures of modern lake sediments of western India, and its palaeo-environmental implications
Open AccessAnjali Trivedi, Sheikh Nawaz Ali et al.ARTICLEQuaternary International2024
Monitoring hydroecology and climatic variability since ~4.6 ka from palynological, sedimentological and environmental perspectives in an Ox-bow lake, Central Ganga Plain, India
Open AccessAnjum Farooqui, Salman Khan et al.ARTICLEThe Holocene2023Referências: 13
The Ganga-Sai River Interfluve contains several ox-bow lakes in the fertile Central Ganga plains (CGP). A ~2.20-meter deep sedimentary profile obtained near the Chandra Shekhar Azad bird sanctuary (Nawabganj lake-NL) of the CGP was studied to understand the evolution of the ecosystem and climate using pollen/spores, diatoms, testate amoebae, environmental magnetic data,and carbon and nitrogen isotopes. This sedimentary profile is chronologically …
Spatio-temporal climatic variations during the last five millennia in the Ladakh Himalaya (India) and its links to archaeological finding(s) (including coprolites) in a palaeoecological and palaeoenvi…
Open AccessBinita Phartiyal, Vivesh V Kapur et al.ARTICLEQuaternary International2021
Hydro-climatic variability during last five thousand years and its impact on human colonization and cultural transition in Ladakh sector, India
Open AccessPriyanka Joshi, Binita Phartiyal et al.ARTICLEQuaternary International2021
Holocene paleoenvironmental changes in the marginal marine basin of Great Rann of Kachchh, western India
Open AccessAbhishek Kumar, D M Maurya et al.ARTICLEQuaternary International2021
Caves as interim-refugia
Open AccessAmritpal Singh Chaddha, Runcie Paul Mathews et al.ARTICLEJournal of Archaeological Science…2021Referências: 5
A new chronology based on OSL and radiocarbon dating for the archaeological settlements of Vadnagar (western India) along with magnetic and isotopic imprints of cultural sediments
Open AccessRajesh Agnihotri, Nikhil Patel et al.ARTICLEJournal of Archaeological Science…2021Referências: 8
Holocene hydroclimatic variability in the Zanskar Valley, Northwestern Himalaya, India
Open AccessSheikh Nawaz Ali, Shailesh Agrawal et al.ARTICLEQuaternary Research2020
A 1.3-m-long sediment core from the Penzi-la pass, Zanskar Valley, provides a record of hydroclimatic conditions and abrupt climate changes over short time scales since the mid-Holocene. These climatic changes of centennial time scale are crucial to understanding the hydroclimatic variability in northwestern (NW) Himalaya. Relatively higher δ 13 C values complemented by total organic carbon, loss on ignition, grain size parameters, and lower Rubi…
Environmental magnetic, Geochemical and Sulfur isotopic imprints of an Indus archaeological site 4MSR from western India (Rajasthan)
Open AccessShalini Sharma, Amish Kumar et al.ARTICLEQuaternary International2020
Late-Holocene climatic record from a glacial lake in Ladakh range, Trans-Himalaya, India
Open AccessBinita Phartiyal, Randheer Singh et al.ARTICLEThe Holocene2020Citada por: 2Referências: 16
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…
Late Holocene palaeo-environmental change in the Banni Plains, Kachchh, Western India
Open AccessNisarg Makwana, S P Prizomwala et al.ARTICLEQuaternary International2019
Climatic variations and geomorphology of the Indus River valley, between Nimo and Batalik, Ladakh (NW Trans Himalayas) during Late Quaternary
Open AccessDebarati Nag, Binita PhartiyalARTICLEQuaternary International2015
Glacial lakes and geomorphological evolution of Schirmacher Oasis, East Antarctica, during Late Quaternary
Open AccessBinita Phartiyal, Anupam Sharma et al.ARTICLEQuaternary International2011
Late Quaternary climatic changes in the eastern Kumaun Himalaya, India, as deduced from multi-proxy studies
Open AccessBahadur Singh Kotlia, Jaishri Sanwal et al.ARTICLEQuaternary International2010
Evidence of enhanced winter precipitation and the prevalence of a cool and dry climate during the mid to late Holocene in mainland Gujarat, India
Open AccessVandana Prasad, Binita Phartiyal et al.ARTICLEThe Holocene2007Citada por: 4Referências: 2
The Kothiyakhad sedimentary sequence of Mahi estuary in mainland Gujarat, India, contains valuable information on late- to mid-Holocene climatic conditions as inferred by phytolith, palynofacies, magnetic susceptibility and clay mineralogical studies. Three distinct climatic regimes, ie, Phase I, II and III, were established. Phase I (3660—~3400 yr BP) shows a gradual weakening of SW monsoonal activity, though overlapped by enhanced western distu…