Neera Sharma
Biographic Data
| ID | 6572523 |
|---|---|
| NAME | Neera Sharma |
| GIVEN NAMES | Neera |
| FAMILY NAME | Sharma |
| SIGNATURE | SHARMA N |
| AFFILIATIONS | Maharaja Sayajirao University of Baroda |
| ORCID | 0000-0002-2800-4690 |
| VERIFIED | Yes |
| TOTAL WORKS | 1 |
| TOTAL CITATIONS | 4 |
| WORKS AS AUTHOR | 1 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2013 |
| LATEST PUBLICATION YEAR | 2013 |
| H-INDEX | 1 |
Late-Holocene climate in the Lower Narmada valley, Gujarat, western India, inferred using sedimentary carbon and oxygen isotope ratios
We report the late-Holocene climate and vegetation of the Lower Narmada valley, Gujarat, western India as inferred from the stable carbon and oxygen isotopic composition (δ 13 C and δ 18 O) of sedimentary carbonates and the associated organic carbon. The alluvial plain from the surface to a depth of ~2 m consists of late-Holocene sediments, deposited during last ~3 kyr, probably by large historic and paleofloods. δ 13 C of both carbonates and org…
Late-Holocene climate in the Lower Narmada valley, Gujarat, western India, inferred using sedimentary carbon and oxygen isotope ratios
We report the late-Holocene climate and vegetation of the Lower Narmada valley, Gujarat, western India as inferred from the stable carbon and oxygen isotopic composition (δ 13 C and δ 18 O) of sedimentary carbonates and the associated organic carbon. The alluvial plain from the surface to a depth of ~2 m consists of late-Holocene sediments, deposited during last ~3 kyr, probably by large historic and paleofloods. δ 13 C of both carbonates and org…
Late-Holocene climate in the Lower Narmada valley, Gujarat, western India, inferred using sedimentary carbon and oxygen isotope ratios
We report the late-Holocene climate and vegetation of the Lower Narmada valley, Gujarat, western India as inferred from the stable carbon and oxygen isotopic composition (δ 13 C and δ 18 O) of sedimentary carbonates and the associated organic carbon. The alluvial plain from the surface to a depth of ~2 m consists of late-Holocene sediments, deposited during last ~3 kyr, probably by large historic and paleofloods. δ 13 C of both carbonates and org…
Alluvium (1 work) · Climate change (1 work) · Ecology (1 work) · Geography (1 work) · Geological formations and processes (1 work) · Geology (1 work) · Geology and Paleoclimatology Research (1 work) · Holocene (1 work) · Holocene climatic optimum (1 work) · Isotope Analysis in Ecology (1 work)