Environmental conditions during freezing, and response of microbial mats in ponds of the McMurdo Ice Shelf, Antarctica

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 condition...

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Published in:Antarctic Science
Main Authors: Hawes, I., Smith, R., Howard-Williams, C., Schwarz, A-M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1999
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102099000267
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102099000267
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spelling crcambridgeupr:10.1017/s0954102099000267 2024-09-15T17:44:39+00:00 Environmental conditions during freezing, and response of microbial mats in ponds of the McMurdo Ice Shelf, Antarctica Hawes, I. Smith, R. Howard-Williams, C. Schwarz, A-M. 1999 http://dx.doi.org/10.1017/s0954102099000267 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102099000267 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 11, issue 2, page 198-208 ISSN 0954-1020 1365-2079 journal-article 1999 crcambridgeupr https://doi.org/10.1017/s0954102099000267 2024-08-07T04:01:36Z 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. Article in Journal/Newspaper Antarc* Antarctic Science Antarctica Ice Shelf McMurdo Ice Shelf Cambridge University Press Antarctic Science 11 2 198 208
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description 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.
format Article in Journal/Newspaper
author Hawes, I.
Smith, R.
Howard-Williams, C.
Schwarz, A-M.
spellingShingle Hawes, I.
Smith, R.
Howard-Williams, C.
Schwarz, A-M.
Environmental conditions during freezing, and response of microbial mats in ponds of the McMurdo Ice Shelf, Antarctica
author_facet Hawes, I.
Smith, R.
Howard-Williams, C.
Schwarz, A-M.
author_sort Hawes, I.
title Environmental conditions during freezing, and response of microbial mats in ponds of the McMurdo Ice Shelf, Antarctica
title_short Environmental conditions during freezing, and response of microbial mats in ponds of the McMurdo Ice Shelf, Antarctica
title_full Environmental conditions during freezing, and response of microbial mats in ponds of the McMurdo Ice Shelf, Antarctica
title_fullStr Environmental conditions during freezing, and response of microbial mats in ponds of the McMurdo Ice Shelf, Antarctica
title_full_unstemmed Environmental conditions during freezing, and response of microbial mats in ponds of the McMurdo Ice Shelf, Antarctica
title_sort environmental conditions during freezing, and response of microbial mats in ponds of the mcmurdo ice shelf, antarctica
publisher Cambridge University Press (CUP)
publishDate 1999
url http://dx.doi.org/10.1017/s0954102099000267
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102099000267
genre Antarc*
Antarctic Science
Antarctica
Ice Shelf
McMurdo Ice Shelf
genre_facet Antarc*
Antarctic Science
Antarctica
Ice Shelf
McMurdo Ice Shelf
op_source Antarctic Science
volume 11, issue 2, page 198-208
ISSN 0954-1020 1365-2079
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0954102099000267
container_title Antarctic Science
container_volume 11
container_issue 2
container_start_page 198
op_container_end_page 208
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