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.Základní údaje
Originální název
Unusual biogenic calcite structures in two shallow lakes, James Ross Island, Antarctica
Autoři
ELSTER, Josef (203 Česká republika, garant), Linda NEDBALOVÁ (203 Česká republika), Radek VODRÁŽKA (203 Česká republika), Kamil LÁSKA (203 Česká republika, domácí), Jakub HALODA (203 Česká republika) a Jiří KOMÁREK (203 Česká republika)
Vydání
Biogeosciences, 2016, 1726-4170
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10600 1.6 Biological sciences
Stát vydavatele
Německo
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 3.851
Kód RIV
RIV/00216224:14310/16:00089157
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000369524500014
Klíčová slova anglicky
Antarctica; James Ross Island; lakes; photoautotrophic mat; calcite spicules
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 14. 4. 2017 21:29, Ing. Andrea Mikešková
Anotace
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.
Návaznosti
LM2010009, projekt VaV |
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MUNI/A/1370/2014, interní kód MU |
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