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Amzad H. Laskar

Researcher at Physical Research Laboratory

Publications -  49
Citations -  787

Amzad H. Laskar is an academic researcher from Physical Research Laboratory. The author has contributed to research in topics: Monsoon & Holocene. The author has an hindex of 15, co-authored 45 publications receiving 569 citations. Previous affiliations of Amzad H. Laskar include Utrecht University & Academia Sinica.

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InterCarb: A Community Effort to Improve Interlaboratory Standardization of the Carbonate Clumped Isotope Thermometer Using Carbonate Standards.

Stefano M. Bernasconi, +73 more
TL;DR: In this paper, the authors provide consensus values from the clumped isotope community for four carbonate standards relative to heated and equilibrated gases with 1,819 individual analyses from 10 laboratories.
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A 4 kyr stalagmite oxygen isotopic record of the past Indian Summer Monsoon in the Andaman Islands

TL;DR: In this article, two stalagmites from Baratang cave in Andaman Islands have been investigated for their temporal variations in δ18O to reconstruct the activity of the Indian Summer Monsoon (ISM) during the last ∼4 kyr.
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Oxygen, deuterium, and strontium isotope characteristics of the Indus River water system

TL;DR: In this paper, stable isotopic compositions (δD and δ18O) and strontium isotopic ratio (87Sr/86Sr) in the Indus River water, its tributaries and its small streams (nallahs) were used to understand the regional hydrology, water sources, and catchment processes.
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Late-Holocene climate in the Lower Narmada valley, Gujarat, western India, inferred using sedimentary carbon and oxygen isotope ratios:

TL;DR: This article reported the late-Holocene climate and vegetation of the Lower Narmada valley, Gujarat, western India as inferred from the stable carbon and oxygen isotopic composition (δ13C and δ18O) of sediment.
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Zonal variability in primary production and nitrogen uptake rates in the southwestern Indian Ocean and the Southern Ocean

TL;DR: In this paper, primary and new production measurements were carried out during the austral summer of 2009, in the southwestern Indian Ocean and Indian sector of the Southern Ocean (SO) in different zones of SO, and the results showed that the maximum possible f -ratio in SO could be as high as 0.78±0.12 and under such conditions the region could export most of the total production to the deep.