Md Firoze Quamar
Dados Biográficos
| ID | 6571122 |
|---|---|
| NOME | Md Firoze Quamar |
| PRENOMES | Md Firoze |
| SOBRENOME | Quamar |
| ASSINATURA | QUAMAR M F |
| AFILIAÇÕES | Birbal Sahni Institute of Palaeosciences |
| ORCID | 0000-0002-3087-2008 |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 10 |
| TOTAL DE CITAÇÕES | 14 |
| TOTAL COMO AUTOR | 10 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 2014 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2026 |
| ÍNDICE H | 3 |
Vegetation dynamics, corresponding climate change and Indian Summer Monsoon variability during the Middle-to Late Holocene from the Core Monsoon Zone, India
Evaluating the Indian Summer Monsoon intensity using archeological seeds from early–late historic Vidarbha, Central India
We present an archaeobotanical record representing ~2300 years BP farming practice at Nagardhan an Early Historic—Late Medieval site in the Vidarbha region, Maharashtra, central India. The study assesses the crop harvesting patterns and Indian Summer Monsoon (ISM) intensity using two different approaches (archaeobotany, and canonical correspondence analysis) to understand the variability and impact of ISM on human subsistence systems during perio…
Late Quaternary climate reconstruction using multiproxy approach and mathematical techniques
Vegetation Response to the Hydro-Climatic Changes During the Late Quaternary
Climate change is most clearly reflected in vegetation, as it forms an integral and fundamental component of ecosystems that is sensitive to and governed by climatic changes [...]
Vegetation diversity in response to monsoonal variability in the Eastern Himalaya, India over the past ~13 000 yrs
Monsoon precipitation plays a crucial role in shaping the diversity of vegetation in the Himalayas, both in terms of temporal and spatial distribution. While palynology has traditionally been employed to reconstruct the past climate of the Himalaya, there has been limited understanding of how monsoon-related changes affect the structure and distribution of vegetation. To address this, we analysed pollen data from a 3 m deep sedimentary profile in…
Vegetation Dynamics and Hydro-Climatic Changes during the Middle Holocene from the Central Himalaya, India
Understanding the spatiotemporal monsoonal variability during the Holocene helps in understanding the rise and fall of many civilizations. In this study, a 2.65 m high palaeo lake sedimentary profile from the Kumaun Lesser Himalaya, Uttarakhand State, India was pollen analysed to reconstruct the variability in the monsoonal precipitation during the Middle Holocene. The study revealed that between ~7522 and 7216 cal yr BP, conifers dominated mixed…
Agricultural practices in India during the Holocene
Pollen assemblages provide valuable insights into the beginning of cereal-based agricultural practices and the transition from a hunting and gathering to a sedentary and food-producing way of life. Anthropogenic pollen indicators (APIs) and their precise identification, with respect to taxonomic resolution, can help to document the history of agricultural development, pastoral activities and human-induced land-use changes, particularly for the Ho…
Vegetation response to the Indian Summer Monsoon (ISM) variability during the Late-Holocene from the central Indian core monsoon zone
Pollen analysis and radiocarbon dating of a 1.4 m deep lacustrine sediment profile from Chhattisgarh State, central India, in the core monsoon zone (CMZ), has revealed the vegetation history, associated climate change and the Indian Summer Monsoon (ISM) rainfall variability during the Late-Holocene. The pollen evidence suggests that between ca. 3000 and 2600 cal year BP, tree-savannah vegetation occurred in the region having a comparatively lesse…
Vegetation dynamics in response to climate change from the wetlands of Western Himalaya, India
India’s agricultural output, economy and societal well-being are strappingly dependent on the stability of the southwest summer monsoon precipitation, its variability and extremes. Deviations in the Indian summer monsoon (ISM) precipitation may profoundly impact the agricultural productivity and gross domestic product (GDP) of the country. Understanding the spatiotemporal dynamics of the ISM precipitation during the Holocene is significant in man…
Pollen production and depositional behaviour of teak (Tectona grandis Linn. F.) and sal (Shorea robusta Gaertn. F.) in tropical deciduous forests of Madhya Pradesh, India
Vegetation response to the Indian Summer Monsoon (ISM) variability during the Late-Holocene from the central Indian core monsoon zone
Pollen analysis and radiocarbon dating of a 1.4 m deep lacustrine sediment profile from Chhattisgarh State, central India, in the core monsoon zone (CMZ), has revealed the vegetation history, associated climate change and the Indian Summer Monsoon (ISM) rainfall variability during the Late-Holocene. The pollen evidence suggests that between ca. 3000 and 2600 cal year BP, tree-savannah vegetation occurred in the region having a comparatively lesse…
Vegetation dynamics in response to climate change from the wetlands of Western Himalaya, India
India’s agricultural output, economy and societal well-being are strappingly dependent on the stability of the southwest summer monsoon precipitation, its variability and extremes. Deviations in the Indian summer monsoon (ISM) precipitation may profoundly impact the agricultural productivity and gross domestic product (GDP) of the country. Understanding the spatiotemporal dynamics of the ISM precipitation during the Holocene is significant in man…
Agricultural practices in India during the Holocene
Pollen assemblages provide valuable insights into the beginning of cereal-based agricultural practices and the transition from a hunting and gathering to a sedentary and food-producing way of life. Anthropogenic pollen indicators (APIs) and their precise identification, with respect to taxonomic resolution, can help to document the history of agricultural development, pastoral activities and human-induced land-use changes, particularly for the Ho…
Pollen production and depositional behaviour of teak (Tectona grandis Linn. F.) and sal (Shorea robusta Gaertn. F.) in tropical deciduous forests of Madhya Pradesh, India
Vegetation dynamics in response to climate change from the wetlands of Western Himalaya, India
India’s agricultural output, economy and societal well-being are strappingly dependent on the stability of the southwest summer monsoon precipitation, its variability and extremes. Deviations in the Indian summer monsoon (ISM) precipitation may profoundly impact the agricultural productivity and gross domestic product (GDP) of the country. Understanding the spatiotemporal dynamics of the ISM precipitation during the Holocene is significant in man…
Vegetation response to the Indian Summer Monsoon (ISM) variability during the Late-Holocene from the central Indian core monsoon zone
Pollen analysis and radiocarbon dating of a 1.4 m deep lacustrine sediment profile from Chhattisgarh State, central India, in the core monsoon zone (CMZ), has revealed the vegetation history, associated climate change and the Indian Summer Monsoon (ISM) rainfall variability during the Late-Holocene. The pollen evidence suggests that between ca. 3000 and 2600 cal year BP, tree-savannah vegetation occurred in the region having a comparatively lesse…
Agricultural practices in India during the Holocene
Pollen assemblages provide valuable insights into the beginning of cereal-based agricultural practices and the transition from a hunting and gathering to a sedentary and food-producing way of life. Anthropogenic pollen indicators (APIs) and their precise identification, with respect to taxonomic resolution, can help to document the history of agricultural development, pastoral activities and human-induced land-use changes, particularly for the Ho…
Vegetation Dynamics and Hydro-Climatic Changes during the Middle Holocene from the Central Himalaya, India
Understanding the spatiotemporal monsoonal variability during the Holocene helps in understanding the rise and fall of many civilizations. In this study, a 2.65 m high palaeo lake sedimentary profile from the Kumaun Lesser Himalaya, Uttarakhand State, India was pollen analysed to reconstruct the variability in the monsoonal precipitation during the Middle Holocene. The study revealed that between ~7522 and 7216 cal yr BP, conifers dominated mixed…
Vegetation diversity in response to monsoonal variability in the Eastern Himalaya, India over the past ~13 000 yrs
Monsoon precipitation plays a crucial role in shaping the diversity of vegetation in the Himalayas, both in terms of temporal and spatial distribution. While palynology has traditionally been employed to reconstruct the past climate of the Himalaya, there has been limited understanding of how monsoon-related changes affect the structure and distribution of vegetation. To address this, we analysed pollen data from a 3 m deep sedimentary profile in…
Vegetation Response to the Hydro-Climatic Changes During the Late Quaternary
Climate change is most clearly reflected in vegetation, as it forms an integral and fundamental component of ecosystems that is sensitive to and governed by climatic changes [...]
Vegetation dynamics, corresponding climate change and Indian Summer Monsoon variability during the Middle-to Late Holocene from the Core Monsoon Zone, India
Evaluating the Indian Summer Monsoon intensity using archeological seeds from early–late historic Vidarbha, Central India
We present an archaeobotanical record representing ~2300 years BP farming practice at Nagardhan an Early Historic—Late Medieval site in the Vidarbha region, Maharashtra, central India. The study assesses the crop harvesting patterns and Indian Summer Monsoon (ISM) intensity using two different approaches (archaeobotany, and canonical correspondence analysis) to understand the variability and impact of ISM on human subsistence systems during perio…
Late Quaternary climate reconstruction using multiproxy approach and mathematical techniques
Geology and Paleoclimatology Research (8 obras) · Climate change (6 obras) · Geography (6 obras) · Holocene (6 obras) · Monsoon (6 obras) · Vegetation (pathology (6 obras) · Biology (5 obras) · Geology (5 obras) · Physical geography (5 obras) · Pollen (5 obras)