Open AccessPaleoenvironments of a proglacial lake in Schirmacher Oasis, East Antarctica: Insights from quartz grain microtextures
Author(s) -
Abhijit Mazumder,
Pawan Govil,
Ratan Kar,
Narath Meethal Gayathri,
Raghuram
Publication year - 2017
Publication title -
polish polar research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.421
H-Index - 32
eISSN - 2081-8262
pISSN - 0138-0338
DOI - 10.1515/popore-2017-0002
Subject(s) - geology , holocene , aeolian processes , quartz , interglacial , glacial period , sediment , quaternary , physical geography , oceanography , geochemistry , geomorphology , paleontology , geography
Eighteen sediment samples from a 36 cm long sediment core retrieved from a proglacial lake (namely P 11) situated in the Schirmacher Oasis, East Antarctica, were analysed for the study of quartz grain morphology and microtexture, along with sand percentage, to reconstruct the paleoenvironmental changes in the lake during the Holocene. The age of the core ranges from 3.3 ka BP to 13.9 ka BP. The quartz grain morphology and microtexture reveal significant evidences of glacial transport along with some eolian and aqueous activities. On the basis of predominance of these signatures and the zonation from CONISS Cluster Analysis on the percentages of characteristic grain morphology and microtextures, the entire core has been subdivided into three major zones. From the paleoenvironmental perspective, it can be concluded that there is an onset of interglacial period at the advent of Holocene (12.3 ka BP), which reigned until 5.3 ka BP and thereafter, again a glacial environment prevailed until 3.3 ka BP with some variations in-between. The results indicate probable alternative colder and less colder phases in the study area, which are also well supported by the respective sand percentages in the sediments