scholarly journals Prokaryotic diversity of arctic ice shelf microbial mats

2008 ◽  
Vol 10 (4) ◽  
pp. 950-966 ◽  
Author(s):  
Eric M. Bottos ◽  
Warwick F. Vincent ◽  
Charles W. Greer ◽  
Lyle G. Whyte
Polar Biology ◽  
2021 ◽  
Author(s):  
Eleanor E. Jackson ◽  
Ian Hawes ◽  
Anne D. Jungblut

AbstractThe undulating ice of the McMurdo Ice Shelf, Southern Victoria Land, supports one of the largest networks of ice-based, multiyear meltwater pond habitats in Antarctica, where microbial mats are abundant and contribute most of the biomass and biodiversity. We used 16S rRNA and 18S rRNA gene high-throughput sequencing to compare variance of the community structure in microbial mats within and between ponds with different salinities and pH. Proteobacteria and Cyanobacteria were the most abundant phyla, and composition at OTU level was highly specific for the meltwater ponds with strong community sorting along the salinity gradient. Our study provides the first detailed evaluation of eukaryote communities for the McMurdo Ice Shelf using the 18S rRNA gene. They were dominated by Ochrophyta, Chlorophyta and Ciliophora, consistent with previous microscopic analyses, but many OTUs belonging to less well-described heterotrophic protists from Antarctic ice shelves were also identified including Amoebozoa, Rhizaria and Labyrinthulea. Comparison of 16S and 18S rRNA gene communities showed that the Eukaryotes had lower richness and greater similarity between ponds in comparison with Bacteria and Archaea communities on the McMurdo Ice shelf. While there was a weak correlation between community dissimilarity and geographic distance, the congruity of microbial assemblages within ponds, especially for Bacteria and Archaea, implies strong habitat filtering in ice shelf meltwater pond ecosystems, especially due to salinity. These findings help to understand processes that are important in sustaining biodiversity and the impact of climate change on ice-based aquatic habitats in Antarctica.


2010 ◽  
Vol 29 (25-26) ◽  
pp. 3590-3597 ◽  
Author(s):  
F. Colleoni ◽  
G. Krinner ◽  
M. Jakobsson
Keyword(s):  

ARCTIC ◽  
1960 ◽  
Vol 13 (1) ◽  
Author(s):  
A.P. Crary
Keyword(s):  

1987 ◽  
Vol 9 ◽  
pp. 145-150 ◽  
Author(s):  
Martin O. Jeffries ◽  
William M. Sackinger ◽  
Harold V. Serson

Periodically since 1950, air photographs and SLAR images have been taken of the Arctic ice shelves. The study of air photographs and SLAR images of the outer part of Milne Ice Shelf had three aims: (1) to map losses and ice re-growth at the shelf front, (2) to map the evolution of melt pools on shelf ice and multi-year land-fast sea ice, and (3) to assess the usefulness of air photographs and SLAR for these purposes. For mapping of ice calvings and subsequent sea-ice growth, both air photographs and radar images have been used sucessfully. However, air photographs are better than radar for mapping ice-surface features. The ridge-and-trough systems that characterize the surface of the ice shelf and old sea ice are clearly visible on each type of imagery but, because of their larger scale, air photographs proved to be most useful for a study of melt-pool evolution. The orientation of the melt pools is parallel to the prevailing winds which drive water along the troughs. The drainage system evolves by a process of elongation and coalesence.


1999 ◽  
Vol 11 (2) ◽  
pp. 198-208 ◽  
Author(s):  
I. Hawes ◽  
R. Smith ◽  
C. Howard-Williams ◽  
A-M. Schwarz

Environmental conditions, both external to and within three shallow ponds of the McMurdo Ice Shelf, were measured over an annual cycle between January 1997 and January 1998. We combined this with a study of the response of the benthic microbial mat communities to the transition from summer conditions to winter freezing. Over the study period air temperature was above 0°C for a few days during summer. At this time pond temperatures were higher than air temperatures, with evidence of thermo-haline stratification. The shallow areas of ponds froze between late February and early March, with bottom waters in the deepest pond remaining unfrozen until early June. Minimum winter air temperatures were below −40°C. There was little evidence of freezing point depression due to freeze-concentration of solutes, except at the very bottom of ponds. In the most conductive pond investigated, the temperature of basal freezing was −4°C and conductivity did not exceed approximately 60 mS cm−1 immediately prior to freezing. Microbial mats remained photosynthetically active up to conductivities between 40 and 80 mS cm−1, and were able to acclimate to lowered irradiance associated with ice formation. Although photosynthesis and respiration were reduced by 11% and 40% respectively at temperatures of −2°C compared to 1°C, there was no difference in light harvesting efficiency. Results from this study suggest that light limitation of photosynthesis, or freezing, determine the growth season for the microbial communities, depending on depth.


2003 ◽  
Vol 30 (20) ◽  
Author(s):  
Derek R. Mueller ◽  
Warwick F. Vincent ◽  
Martin O. Jeffries
Keyword(s):  
Break Up ◽  

2009 ◽  
Vol 40 (2) ◽  
pp. 258-269 ◽  
Author(s):  
Anne D. Jungblut ◽  
Michelle A. Allen ◽  
Brendan P. Burns ◽  
Brett A. Neilan

Nature ◽  
2016 ◽  
Vol 530 (7589) ◽  
pp. 163-164 ◽  
Author(s):  
Eugene Domack
Keyword(s):  

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