Indian summer monsoon variability and vegetation changes in the core monsoon zone, India, during the Holocene
A multiproxy study
Dados Bibliográficos
| ID | 12267161 |
|---|---|
| Autores | Kamlesh Kumar (0000-0001-8713-3938, Birbal Sahni Institute of Palaeosciences, autor correspondente), Shailesh Agrawal (Birbal Sahni Institute of Palaeosciences), Anupam Sharma (0000-0001-7872-5827, Birbal Sahni Institute of Palaeosciences), Shilpa Pandey (Birbal Sahni Institute of Palaeosciences) |
| Ano | 2018 |
| Volume | 29 |
| Fascículo | 1 |
| Páginas | 110-119 |
| Data de publicação | 2018-10-12 |
| Peer Reviewed | Sim |
| Open Access | Sim |
| Tipo | ARTICLE |
| Periódico | The Holocene (JOURNAL) |
| Identificadores do periódico | ISSN: 0959-6836 • E-ISSN: 1477-0911 |
| Editora | SAGE Publishing (PUBLISHER • US) |
| DOI | 10.1177/0959683618804641 |
| OpenAlex | W2897881941 |
| Idioma | EN |
| Citações recebidas | 9 |
| Referências citadas | 62 |
We present the results of sediment texture, δ 13 C values, TOC, TN, TOC/TN, and magnetic susceptibility (χ lf ) of a 1.54-m deep sediment trench recovered from the core monsoon zone (CMZ) of central India, to understand the paleovegetational history and Indian summer monsoon (ISM) variability during the Holocene. The lower δ 13 C values, TOC/TN ratio, and magnetic susceptibility (χ lf ) from ~11.4 to 9.5 ka BP suggest enhanced ISM intensity, which is well correlated with other available ISM records from both terrestrial as well as marine archives. A gradual stepwise expansion of C 4 plants during ~8.1 and 6.3 ka BP, ~6.3 to 4.7 ka BP, and ~3.0 to 2.0 ka BP suggests a gradual weakening of ISM. The highest δ 13 C values (–18.7‰) recorded at ~2.0 ka BP indicate the dominance of C 4 plants suggesting the weakest phase of ISM in the study area. The expansion of C 3 plants from ~2.0 to 1.6 ka BP indicates a sudden increase in ISM intensity. Subsequently, three stages of enhanced ISM have been recorded between ~1.6 and 0.93 ka BP, ~0.76 and 0.42 ka BP, and ~0.28 ka BP to present
Dominance (genetics · Geography · Holocene · Monsoon · Monsoon of South Asia · Physical geography · Sediment · Chemistry · Geological formations and processes · Geology and Paleoclimatology Research · Geomagnetism and Paleomagnetism Studies · Geology · Oceanography · Paleontology
Holocene hydroclimatic variability in the Zanskar Valley, Northwestern Himalaya, India
Implications for catchment weathering, provenance, and climatic records from a late Pleistocene to present sedimentary sequence in Gujarat, India
Tracing palaeoecological footprints of Late Holocene monsoon variability and vegetation dynamics in the tropical sal forest of India’s Core Monsoon Zone
Paleorainfall during the past two millennia in the Western Ghats, south-western India
Investigating possible links between Holocene environmental changes and cultural transitions across India
New evidence of mid- to late- Holocene vegetation and climate change from a Neolithic settlement in western fringe of Central Ganga Plain
Palaeoclimatic Signatures Based on Pollen Fingerprints
Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas
Increasing frequency of extreme climatic events in southern India during the Late Holocene
Timing, cause and consequences of mid-Holocene climate transition in the Arabian Sea
Paleoclimatic Significance of the Mineral Magnetic Record of the Chinese Loess and Paleosols
Variability of Indian monsoonal rainfall over the past 100 ka and its implication for C 3 –C 4 vegetational change
Estimates of Holocene Precipitation for Rajasthan, India, Based on Pollen and Lake-Level Data
Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean
Prolonged monsoon droughts and links to Indo-Pacific warm pool
Holocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman
High-Resolution Holocene Environmental Changes in the Thar Desert, Northwestern India
Preservation of elemental and isotopic source identification of sedimentary organic matter
Tropical Climate Instability
A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China
The Asian monsoon over the past 640,000 years and ice age terminations
Organic geochemical proxies of paleoceanographic, paleolimnologic, and paleoclimatic processes
Climate change at the 4.2 ka BP termination of the Indus valley civilization and Holocene south Asian monsoon variability
Carbon Isotopes in Photosynthesis
The variation of summer monsoon precipitation in central China since the last deglaciation
Holocene environmental changes in Bangong Co basin (Western Tibet). Part 4
Century-scale events in monsoonal climate over the past 24,000 years
Holocene Paleoclimates of India
Lacustrine organic geochemistry—an overview of indicators of organic matter sources and diagenesis in lake sediments
Late Quaternary vegetation history, climatic variability and human activity in the Central Ganga Plain, deduced by pollen proxy records from Karela Jheel, India
Lipid distribution in the lake Ennamangalam, south India
A Holocene pollen record from the northwestern Himalayan lake Tso Moriri
Early-Holocene to present palaeoenvironmental shifts and short climate events from the tropical wetland and lake sediments, Kukkal Lake, Southern India
Extended 14 C Data Base and Revised Calib 3.0 14 C Age Calibration Program
| Obras citantes distintas | 9 |
|---|---|
| Citações por ano | 1,5 |
| Intervalo de citações | 2020 - 2026 (7) |
| Velocidade de citação | current |
| Altamente citado | Não |
| Tipos de citação | Neutras: 6 |