Winter Phytoplankton Densities 1990-1991

Using automated overwinter sampling devices, preserved phytoplankton samples were collected from multiple depths in Lake Fryxell, a permanently ice-covered lake in southern Victoria Land, Antarctica. Photosynthetic algae (i.e. algae possessing chloroplasts) are maintained in a stable water column th...

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Format: Dataset
Language:unknown
Published: McMurdo Dry Valleys LTERByrd Polar Research Center 108 Scott Hall1090 Carmack RdColumbusColumbusOH43210-1002USA(614) 292-4697 2011
Subjects:
Online Access:http://hdl.handle.net/10255/dryad.14631
http://metacat.lternet.edu/knb/metacat/knb-lter-mcm.0049.2/xml
id ftdryad:oai:v1.datadryad.org:10255/dryad.14631
record_format openpolar
institution Open Polar
collection Dryad Digital Repository (Duke University)
op_collection_id ftdryad
language unknown
topic lake
limnology
phytoplankton
density
phylum
spellingShingle lake
limnology
phytoplankton
density
phylum
Winter Phytoplankton Densities 1990-1991
topic_facet lake
limnology
phytoplankton
density
phylum
description Using automated overwinter sampling devices, preserved phytoplankton samples were collected from multiple depths in Lake Fryxell, a permanently ice-covered lake in southern Victoria Land, Antarctica. Photosynthetic algae (i.e. algae possessing chloroplasts) are maintained in a stable water column throughout winter darkness. The algal taxa "overwinter" in different ways, in a species specific manner. Typical vegetative cells were the most abundant form for all species found in the water column. Populations of one chlorophyte, Stichococcus sp., and two cryptophyte species increased during winter. We interpret the increase in algal population size as evidence of wintertime heterotrophic growth, and mixotrophic behavior in the context of the entire year. For two chlorophyte species some portion of the population had distinct morphology, e.g. akinetes for Chlamydomonas subcaudata and cells containing a large amount of starch or other storage material for Chlorella sp. During winter, vegetative cells of the most abundant species of cyanobacteria, Phormidium angustissimum, occurred at the depth of the summertime maximum and at depths below the oxycline, which may represent a "false bottom". Other than this false bottom and the absence of diatoms, settling did not appear to influence the overwintering algal community.
format Dataset
title Winter Phytoplankton Densities 1990-1991
title_short Winter Phytoplankton Densities 1990-1991
title_full Winter Phytoplankton Densities 1990-1991
title_fullStr Winter Phytoplankton Densities 1990-1991
title_full_unstemmed Winter Phytoplankton Densities 1990-1991
title_sort winter phytoplankton densities 1990-1991
publisher McMurdo Dry Valleys LTERByrd Polar Research Center 108 Scott Hall1090 Carmack RdColumbusColumbusOH43210-1002USA(614) 292-4697
publishDate 2011
url http://hdl.handle.net/10255/dryad.14631
http://metacat.lternet.edu/knb/metacat/knb-lter-mcm.0049.2/xml
op_coverage Lake Fryxell is located in Taylor Valley in the McMurdo Dry Valleys of southern Victoria Land, Antarctica. The McMurdo Dry Valleys is the largest of the desert oases on the Antarctic coast and is located in the Transantarctic Mountains along the western edge of McMurdo Sound. The valleys run perpendicular to the coast and contain numerous perennially ice-covered lakes. Lake Fryxell is fed by nine major inflow streams which drain Canada and Commonwealth Glaciers and glaciers in the Kukri Hills. The streams are neutral pH and range in conductivity from 23 uS to 200 uS, with solutes accrued by dissolution of marine aerosols, calcite and primary weathering of silicate rocks. Nutrients are gained through weathering of apatite and dissolution of nitrate from atmospheric deposition. Lower nutrient concentrations occur in streams with abundant algal mats. Streamwater DOC concentrations are as high as 9 mg C/L during the initial flow and then decrease to 1 mg C/L or less. Fulvic acid accounts for only 7-10% of streamwater DOC, suggesting that streamflow may contribute labile organic substrates to the lake. The annual cycle of dry valley ecosystems is controlled by extreme changes between summer and winter. During summer, beginning at the end of October, there is continuous sunlight and temperatures above freezing occur for periods of several days. These summer conditions support growth of photosynthetic algae in the pelagic zone and benthos of the lake, and in many meltwater streams. The winter period of total darkness begins in mid-April and ends in mid-August. The ice-cover protects the lake ecosystem from the extreme winds and cold temperatures of winter. Stream algal mats survive winter in a dormant "freeze-dried" state. In the "spring" (mid-August to late October) and "fall" (mid-February to mid-April) the valleys are in twilight during portions of the day, and air temperatures are warmer than in winter, but always below freezing. In Lake Fryxell, streamflow mixes with a 1-2 m layer just below the ice-cover. Below this layer, the water column is very stable and chemical profiles are consistent with molecular diffusion. The major ions and DOC increase with depth. Bottom waters at 18 m have a salinity of 25% of seawater and a DOC concentration of 30 mg C/L. The DOC profile and high DOC concentration in sediment is a significant DOC source. Fulvic acid accounts for 20-24% of the DOC and the fulvic acid chemistry is uniform except for higher sulfur content at depth. Photosynthesis by phytoplankton begins in September and continues into fall. During summer, about 1% of the surface light penetrates the ice cover and light intensity decreases exponentially to values about 0.3uM/m^2/s at 9 m. In this euphotic zone, O2 concentrations are supersaturated due to freeze out of O2 carried by streamwater and to algal production of O2. A sharp oxycline occurs at about 9.5 m, and below the oxycline H2S concentrations increase with depth.
162 W 163.6 E -77.2 N -77.8 S
1990 to 1991
long_lat ENVELOPE(163.000,163.000,-77.617,-77.617)
ENVELOPE(163.183,163.183,-77.617,-77.617)
ENVELOPE(163.183,163.183,-77.617,-77.617)
ENVELOPE(162.700,162.700,-77.733,-77.733)
geographic Antarctic
The Antarctic
Victoria Land
McMurdo Dry Valleys
McMurdo Sound
Transantarctic Mountains
Canada
Taylor Valley
Fryxell
Lake Fryxell
Kukri Hills
geographic_facet Antarctic
The Antarctic
Victoria Land
McMurdo Dry Valleys
McMurdo Sound
Transantarctic Mountains
Canada
Taylor Valley
Fryxell
Lake Fryxell
Kukri Hills
genre Antarc*
Antarctic
Antarctica
glacier*
McMurdo Dry Valleys
McMurdo Sound
Victoria Land
genre_facet Antarc*
Antarctic
Antarctica
glacier*
McMurdo Dry Valleys
McMurdo Sound
Victoria Land
op_relation http://metacat.lternet.edu/knb/metacat/knb-lter-mcm.0049.2/xml
knb-lter-mcm.0049.2
http://hdl.handle.net/10255/dryad.14631
op_rights MCM LTER data may be used freely with the following restrictions:The Principal Investigator be sent a notice stating reasons for acquiring any data and a description of the publication intentions. The Principal Investigator of the data set be sent a copy of the report or manuscript prior to submission and be adequately cited in any resultant publications.A copy of any resultant publications should be sent to the McMurdo data manager and principal investigator.The end-user follow the guidelines set forth in the LTER Network Data Access Policy, Data Access Requirements, and General Data Use Agreement found at http://www.mcmlter.org/data_guidelines.htm
_version_ 1766258947969253376
spelling ftdryad:oai:v1.datadryad.org:10255/dryad.14631 2023-05-15T13:53:38+02:00 Winter Phytoplankton Densities 1990-1991 Lake Fryxell is located in Taylor Valley in the McMurdo Dry Valleys of southern Victoria Land, Antarctica. The McMurdo Dry Valleys is the largest of the desert oases on the Antarctic coast and is located in the Transantarctic Mountains along the western edge of McMurdo Sound. The valleys run perpendicular to the coast and contain numerous perennially ice-covered lakes. Lake Fryxell is fed by nine major inflow streams which drain Canada and Commonwealth Glaciers and glaciers in the Kukri Hills. The streams are neutral pH and range in conductivity from 23 uS to 200 uS, with solutes accrued by dissolution of marine aerosols, calcite and primary weathering of silicate rocks. Nutrients are gained through weathering of apatite and dissolution of nitrate from atmospheric deposition. Lower nutrient concentrations occur in streams with abundant algal mats. Streamwater DOC concentrations are as high as 9 mg C/L during the initial flow and then decrease to 1 mg C/L or less. Fulvic acid accounts for only 7-10% of streamwater DOC, suggesting that streamflow may contribute labile organic substrates to the lake. The annual cycle of dry valley ecosystems is controlled by extreme changes between summer and winter. During summer, beginning at the end of October, there is continuous sunlight and temperatures above freezing occur for periods of several days. These summer conditions support growth of photosynthetic algae in the pelagic zone and benthos of the lake, and in many meltwater streams. The winter period of total darkness begins in mid-April and ends in mid-August. The ice-cover protects the lake ecosystem from the extreme winds and cold temperatures of winter. Stream algal mats survive winter in a dormant "freeze-dried" state. In the "spring" (mid-August to late October) and "fall" (mid-February to mid-April) the valleys are in twilight during portions of the day, and air temperatures are warmer than in winter, but always below freezing. In Lake Fryxell, streamflow mixes with a 1-2 m layer just below the ice-cover. Below this layer, the water column is very stable and chemical profiles are consistent with molecular diffusion. The major ions and DOC increase with depth. Bottom waters at 18 m have a salinity of 25% of seawater and a DOC concentration of 30 mg C/L. The DOC profile and high DOC concentration in sediment is a significant DOC source. Fulvic acid accounts for 20-24% of the DOC and the fulvic acid chemistry is uniform except for higher sulfur content at depth. Photosynthesis by phytoplankton begins in September and continues into fall. During summer, about 1% of the surface light penetrates the ice cover and light intensity decreases exponentially to values about 0.3uM/m^2/s at 9 m. In this euphotic zone, O2 concentrations are supersaturated due to freeze out of O2 carried by streamwater and to algal production of O2. A sharp oxycline occurs at about 9.5 m, and below the oxycline H2S concentrations increase with depth. 162 W 163.6 E -77.2 N -77.8 S 1990 to 1991 2011-04-21T18:03:26Z text/plain http://hdl.handle.net/10255/dryad.14631 http://metacat.lternet.edu/knb/metacat/knb-lter-mcm.0049.2/xml unknown McMurdo Dry Valleys LTERByrd Polar Research Center 108 Scott Hall1090 Carmack RdColumbusColumbusOH43210-1002USA(614) 292-4697 http://metacat.lternet.edu/knb/metacat/knb-lter-mcm.0049.2/xml knb-lter-mcm.0049.2 http://hdl.handle.net/10255/dryad.14631 MCM LTER data may be used freely with the following restrictions:The Principal Investigator be sent a notice stating reasons for acquiring any data and a description of the publication intentions. The Principal Investigator of the data set be sent a copy of the report or manuscript prior to submission and be adequately cited in any resultant publications.A copy of any resultant publications should be sent to the McMurdo data manager and principal investigator.The end-user follow the guidelines set forth in the LTER Network Data Access Policy, Data Access Requirements, and General Data Use Agreement found at http://www.mcmlter.org/data_guidelines.htm lake limnology phytoplankton density phylum dataset 2011 ftdryad 2020-01-01T14:32:12Z Using automated overwinter sampling devices, preserved phytoplankton samples were collected from multiple depths in Lake Fryxell, a permanently ice-covered lake in southern Victoria Land, Antarctica. Photosynthetic algae (i.e. algae possessing chloroplasts) are maintained in a stable water column throughout winter darkness. The algal taxa "overwinter" in different ways, in a species specific manner. Typical vegetative cells were the most abundant form for all species found in the water column. Populations of one chlorophyte, Stichococcus sp., and two cryptophyte species increased during winter. We interpret the increase in algal population size as evidence of wintertime heterotrophic growth, and mixotrophic behavior in the context of the entire year. For two chlorophyte species some portion of the population had distinct morphology, e.g. akinetes for Chlamydomonas subcaudata and cells containing a large amount of starch or other storage material for Chlorella sp. During winter, vegetative cells of the most abundant species of cyanobacteria, Phormidium angustissimum, occurred at the depth of the summertime maximum and at depths below the oxycline, which may represent a "false bottom". Other than this false bottom and the absence of diatoms, settling did not appear to influence the overwintering algal community. Dataset Antarc* Antarctic Antarctica glacier* McMurdo Dry Valleys McMurdo Sound Victoria Land Dryad Digital Repository (Duke University) Antarctic The Antarctic Victoria Land McMurdo Dry Valleys McMurdo Sound Transantarctic Mountains Canada Taylor Valley ENVELOPE(163.000,163.000,-77.617,-77.617) Fryxell ENVELOPE(163.183,163.183,-77.617,-77.617) Lake Fryxell ENVELOPE(163.183,163.183,-77.617,-77.617) Kukri Hills ENVELOPE(162.700,162.700,-77.733,-77.733)