Detailed Information on Publication Record
2016
Unusual biogenic calcite structures in two shallow lakes, James Ross Island, Antarctica
ELSTER, Josef, Linda NEDBALOVÁ, Radek VODRÁŽKA, Kamil LÁSKA, Jakub HALODA et. al.Basic information
Original name
Unusual biogenic calcite structures in two shallow lakes, James Ross Island, Antarctica
Authors
ELSTER, Josef (203 Czech Republic, guarantor), Linda NEDBALOVÁ (203 Czech Republic), Radek VODRÁŽKA (203 Czech Republic), Kamil LÁSKA (203 Czech Republic, belonging to the institution), Jakub HALODA (203 Czech Republic) and Jiří KOMÁREK (203 Czech Republic)
Edition
Biogeosciences, 2016, 1726-4170
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10600 1.6 Biological sciences
Country of publisher
Germany
Confidentiality degree
není předmětem státního či obchodního tajemství
References:
Impact factor
Impact factor: 3.851
RIV identification code
RIV/00216224:14310/16:00089157
Organization unit
Faculty of Science
UT WoS
000369524500014
Keywords in English
Antarctica; James Ross Island; lakes; photoautotrophic mat; calcite spicules
Tags
International impact, Reviewed
Změněno: 14/4/2017 21:29, Ing. Andrea Mikešková
Abstract
V originále
The floors of two shallow endorheic lakes, located on volcanic surfaces on James Ross Island, are covered with calcareous organosedimentary structures. Their biological and chemical composition, lake water characteristics, and seasonal variability of the thermal regime are introduced. The lakes are frozen down to the bottom for 8–9 months a year and their water chemistry is characterised by low conductivity and neutral to slightly alkaline pH. The photosynthetic microbial mat is composed of filamentous cyanobacteria and microalgae that are considered to be Antarctic endemic species. The mucilaginous black biofilm is covered by green spots formed by a green microalga and the macroscopic structures are packed together with fine material. Thin sections consist of rock substrate, soft biofilm, calcite spicules and mineral grains originating from different sources. The morphology of the spicules is typical of calcium carbonate monocrystals having a layered structure and specific surface texture, which reflect growth and degradation processes. The spicules’ chemical composition and structure correspond to pure calcite. The lakes’ age, altitude, morphometry, geomorphological and hydrological stability, including low sedimentation rates, together with thermal regime predispose the existence of this community. We hypothesise that the precipitation of calcite is connected with the photosynthetic activity of the green microalgae that were not recorded in any other lake in the region. This study has shown that the unique community producing biogenic calcite spicules is quite different to any yet described.
Links
LM2010009, research and development project |
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MUNI/A/1370/2014, interní kód MU |
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