The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes
Two lakes, mesotrophic Heywood Lake and oligotrophicSombre Lake, at Signy Island, have been studied over 1 full yr(1980-1981). The development of deep water anoxia in SombreLake is accompanied by release, from the sediments, of nitrogen,silicon, phosphorus, iron, and manganese. Iron is released from...
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1985
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ftunivtasecite:oai:ecite.utas.edu.au:136970 2023-05-15T13:55:18+02:00 The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes Gallagher, JB 1985 https://www.springer.com/gp/book/9783642822773 https://doi.org/10.1007/9783642822759 http://ecite.utas.edu.au/136970 en eng Springer-Verlag Berlin Heidelberg http://dx.doi.org/10.1007/9783642822759 Gallagher, JB, The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes, Antarctic Nutrient Cycles and Food Webs, Springer-Verlag Berlin Heidelberg, WR Siegfried, PR Condy and RM Laws (ed), Germany, pp. 234-237. ISBN 9783642822773 (1985) [Research Book Chapter] http://ecite.utas.edu.au/136970 Earth Sciences Oceanography Chemical Oceanography Research Book Chapter NonPeerReviewed 1985 ftunivtasecite https://doi.org/10.1007/9783642822759 2020-03-09T23:16:21Z Two lakes, mesotrophic Heywood Lake and oligotrophicSombre Lake, at Signy Island, have been studied over 1 full yr(1980-1981). The development of deep water anoxia in SombreLake is accompanied by release, from the sediments, of nitrogen,silicon, phosphorus, iron, and manganese. Iron is released fromanoxic sediments in massive amounts, but is quickly returnedthrough oxidation to iron oxides, near the anoxic-<>xic boundaryand through possible ferrous carbonate precipitation, within theanoxic region. Phosphorus is also quickly returned to sediments, atthe oxic-anoxic boundary, which suggests efficient co-precipitation-sorptionby the recently oxidized ferrous. Phosphorus is thereforeunable to enter the main waterbody. Melt water inflows are thesource of P supply to the surface waters. Nitrogen and Si appear tohave little association with axides and, therefore, freely pass into theoxic main water-body of the oligotrophic system. There are strongseasonal correlations between the vertical profiles of Fe and P,under the ice cover in Heywood Lake. Nitrogen profiles appearindependent of the other determinants, Si, P, Fe, and Mn. Towardsthe end of the period of bottom-water anoxia, during the springmelt, high concentrations of ferrous, released from the anoxicsediments, have been detected in oxygenated waters. This apparentstability, in the presence of oxygen, may be attributable to a combinationof low pH and the possible influence of high concentrationsof humic acids from the melt inflows. Sulphide concentrations maybecome sufficiently high to influence Fe transport significantly,probably through ferrous sulphide precipitation, within the anoxicregion. Book Part Antarc* Antarctic Signy Island eCite UTAS (University of Tasmania) Antarctic Signy Island ENVELOPE(-45.595,-45.595,-60.708,-60.708) Heywood ENVELOPE(-59.683,-59.683,-62.317,-62.317) Heywood Lake ENVELOPE(-45.609,-45.609,-60.691,-60.691) |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Oceanography Chemical Oceanography |
spellingShingle |
Earth Sciences Oceanography Chemical Oceanography Gallagher, JB The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes |
topic_facet |
Earth Sciences Oceanography Chemical Oceanography |
description |
Two lakes, mesotrophic Heywood Lake and oligotrophicSombre Lake, at Signy Island, have been studied over 1 full yr(1980-1981). The development of deep water anoxia in SombreLake is accompanied by release, from the sediments, of nitrogen,silicon, phosphorus, iron, and manganese. Iron is released fromanoxic sediments in massive amounts, but is quickly returnedthrough oxidation to iron oxides, near the anoxic-<>xic boundaryand through possible ferrous carbonate precipitation, within theanoxic region. Phosphorus is also quickly returned to sediments, atthe oxic-anoxic boundary, which suggests efficient co-precipitation-sorptionby the recently oxidized ferrous. Phosphorus is thereforeunable to enter the main waterbody. Melt water inflows are thesource of P supply to the surface waters. Nitrogen and Si appear tohave little association with axides and, therefore, freely pass into theoxic main water-body of the oligotrophic system. There are strongseasonal correlations between the vertical profiles of Fe and P,under the ice cover in Heywood Lake. Nitrogen profiles appearindependent of the other determinants, Si, P, Fe, and Mn. Towardsthe end of the period of bottom-water anoxia, during the springmelt, high concentrations of ferrous, released from the anoxicsediments, have been detected in oxygenated waters. This apparentstability, in the presence of oxygen, may be attributable to a combinationof low pH and the possible influence of high concentrationsof humic acids from the melt inflows. Sulphide concentrations maybecome sufficiently high to influence Fe transport significantly,probably through ferrous sulphide precipitation, within the anoxicregion. |
format |
Book Part |
author |
Gallagher, JB |
author_facet |
Gallagher, JB |
author_sort |
Gallagher, JB |
title |
The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes |
title_short |
The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes |
title_full |
The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes |
title_fullStr |
The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes |
title_full_unstemmed |
The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes |
title_sort |
influence of iron and manganese on nutrient cycling in shallow freshwater antarctic lakes |
publisher |
Springer-Verlag Berlin Heidelberg |
publishDate |
1985 |
url |
https://www.springer.com/gp/book/9783642822773 https://doi.org/10.1007/9783642822759 http://ecite.utas.edu.au/136970 |
long_lat |
ENVELOPE(-45.595,-45.595,-60.708,-60.708) ENVELOPE(-59.683,-59.683,-62.317,-62.317) ENVELOPE(-45.609,-45.609,-60.691,-60.691) |
geographic |
Antarctic Signy Island Heywood Heywood Lake |
geographic_facet |
Antarctic Signy Island Heywood Heywood Lake |
genre |
Antarc* Antarctic Signy Island |
genre_facet |
Antarc* Antarctic Signy Island |
op_relation |
http://dx.doi.org/10.1007/9783642822759 Gallagher, JB, The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes, Antarctic Nutrient Cycles and Food Webs, Springer-Verlag Berlin Heidelberg, WR Siegfried, PR Condy and RM Laws (ed), Germany, pp. 234-237. ISBN 9783642822773 (1985) [Research Book Chapter] http://ecite.utas.edu.au/136970 |
op_doi |
https://doi.org/10.1007/9783642822759 |
_version_ |
1766261717259517952 |