Abiotic characterization and epilithic communities of a naturally enriched stream at Cierva Point, Antarctic Peninsula
Pingüinera Stream is one of the two main lotic environments of Cierva Point (Antarctic Specially Protected Area No. 134) on the Danco Coast, Antarctic Peninsula. It originates in a large snowfield, flows through a penguin rookery, moss and grass banks, discharging into Cierva Cove. During late Antar...
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ftunibueairesbd:paper:paper_09541020_v17_n2_p163_Mataloni 2023-05-15T13:51:25+02:00 Abiotic characterization and epilithic communities of a naturally enriched stream at Cierva Point, Antarctic Peninsula Mataloni, María Gabriela Vinocur, Alicia Liliana De Tezanos Pinto, Paula 2005 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09541020_v17_n2_p163_Mataloni https://hdl.handle.net/20.500.12110/paper_09541020_v17_n2_p163_Mataloni unknown https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09541020_v17_n2_p163_Mataloni http://hdl.handle.net/20.500.12110/paper_09541020_v17_n2_p163_Mataloni Antarctic streams Ecology Epilithon Freshwater algae Nutrients Taxonomic composition arctic environment community structure freshwater ecosystem Antarctic Peninsula Antarctica Arctic and Antarctic West Antarctica World algae Bryophyta Chamaesiphon subglobosus Chlorophyta Cyanobacteria Cyanobacterium (genus) Leptolyngbya Prasiola calophylla Spheniscidae 2005 ftunibueairesbd https://doi.org/20.500.12110/paper_09541020_v17_n2_p163_Mataloni 2023-02-16T02:12:40Z Pingüinera Stream is one of the two main lotic environments of Cierva Point (Antarctic Specially Protected Area No. 134) on the Danco Coast, Antarctic Peninsula. It originates in a large snowfield, flows through a penguin rookery, moss and grass banks, discharging into Cierva Cove. During late Antarctic summer 2003, we sampled the stream at six locations along its course. Abiotic features characterize it as a clear water system, yet receiving a very high amount of PO4-P and NH4-N from the rookery. These nutrients decrease downstream mainly due to uptake by epilithic algae and oxidation of NH4 + to NO3 -, consequently lowering pH and dissolved O2, which was always under-saturated. Strong correlations between all these parameters support these findings. The epilithic algal community shows both temporal and spatial changes in biomass, composition and relative frequencies. Dominant species at the higher reach of the stream are cyanobacteria, mainly Chamaesiphon subglobosus (Rostafinski) Lemm. and a mesh of Leptolyngbya spp. filaments. The chlorophyta Prasiola calophylla (Carmich.) Menegh. dominates the community in oxygenated, fast-flowing reaches. Comparison with the other main stream from Cierva Point, which is not influenced by the rookery, shows that growth and survival of the epilithic community in this area is limited by factors other than nutrient concentrations. © Antarctic Science Ltd. Fil:Mataloni, G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Vinocur, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:De Tezanos Pinto, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Other/Unknown Material Antarc* Antarctic Antarctic Peninsula Antarctica Arctic West Antarctica Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) Antarctic Antarctic Peninsula Arctic Argentina Cierva ENVELOPE(-60.873,-60.873,-64.156,-64.156) Cierva Cove ENVELOPE(-60.883,-60.883,-64.150,-64.150) Cierva Point ENVELOPE(-60.967,-60.967,-64.150,-64.150) Danco ENVELOPE(-61.033,-61.033,-64.717,-64.717) Danco Coast ENVELOPE(-62.000,-62.000,-64.700,-64.700) Pingüinera ENVELOPE(-60.800,-60.800,-62.450,-62.450) West Antarctica |
institution |
Open Polar |
collection |
Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) |
op_collection_id |
ftunibueairesbd |
language |
unknown |
topic |
Antarctic streams Ecology Epilithon Freshwater algae Nutrients Taxonomic composition arctic environment community structure freshwater ecosystem Antarctic Peninsula Antarctica Arctic and Antarctic West Antarctica World algae Bryophyta Chamaesiphon subglobosus Chlorophyta Cyanobacteria Cyanobacterium (genus) Leptolyngbya Prasiola calophylla Spheniscidae |
spellingShingle |
Antarctic streams Ecology Epilithon Freshwater algae Nutrients Taxonomic composition arctic environment community structure freshwater ecosystem Antarctic Peninsula Antarctica Arctic and Antarctic West Antarctica World algae Bryophyta Chamaesiphon subglobosus Chlorophyta Cyanobacteria Cyanobacterium (genus) Leptolyngbya Prasiola calophylla Spheniscidae Mataloni, María Gabriela Vinocur, Alicia Liliana De Tezanos Pinto, Paula Abiotic characterization and epilithic communities of a naturally enriched stream at Cierva Point, Antarctic Peninsula |
topic_facet |
Antarctic streams Ecology Epilithon Freshwater algae Nutrients Taxonomic composition arctic environment community structure freshwater ecosystem Antarctic Peninsula Antarctica Arctic and Antarctic West Antarctica World algae Bryophyta Chamaesiphon subglobosus Chlorophyta Cyanobacteria Cyanobacterium (genus) Leptolyngbya Prasiola calophylla Spheniscidae |
description |
Pingüinera Stream is one of the two main lotic environments of Cierva Point (Antarctic Specially Protected Area No. 134) on the Danco Coast, Antarctic Peninsula. It originates in a large snowfield, flows through a penguin rookery, moss and grass banks, discharging into Cierva Cove. During late Antarctic summer 2003, we sampled the stream at six locations along its course. Abiotic features characterize it as a clear water system, yet receiving a very high amount of PO4-P and NH4-N from the rookery. These nutrients decrease downstream mainly due to uptake by epilithic algae and oxidation of NH4 + to NO3 -, consequently lowering pH and dissolved O2, which was always under-saturated. Strong correlations between all these parameters support these findings. The epilithic algal community shows both temporal and spatial changes in biomass, composition and relative frequencies. Dominant species at the higher reach of the stream are cyanobacteria, mainly Chamaesiphon subglobosus (Rostafinski) Lemm. and a mesh of Leptolyngbya spp. filaments. The chlorophyta Prasiola calophylla (Carmich.) Menegh. dominates the community in oxygenated, fast-flowing reaches. Comparison with the other main stream from Cierva Point, which is not influenced by the rookery, shows that growth and survival of the epilithic community in this area is limited by factors other than nutrient concentrations. © Antarctic Science Ltd. Fil:Mataloni, G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Vinocur, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:De Tezanos Pinto, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. |
author |
Mataloni, María Gabriela Vinocur, Alicia Liliana De Tezanos Pinto, Paula |
author_facet |
Mataloni, María Gabriela Vinocur, Alicia Liliana De Tezanos Pinto, Paula |
author_sort |
Mataloni, María Gabriela |
title |
Abiotic characterization and epilithic communities of a naturally enriched stream at Cierva Point, Antarctic Peninsula |
title_short |
Abiotic characterization and epilithic communities of a naturally enriched stream at Cierva Point, Antarctic Peninsula |
title_full |
Abiotic characterization and epilithic communities of a naturally enriched stream at Cierva Point, Antarctic Peninsula |
title_fullStr |
Abiotic characterization and epilithic communities of a naturally enriched stream at Cierva Point, Antarctic Peninsula |
title_full_unstemmed |
Abiotic characterization and epilithic communities of a naturally enriched stream at Cierva Point, Antarctic Peninsula |
title_sort |
abiotic characterization and epilithic communities of a naturally enriched stream at cierva point, antarctic peninsula |
publishDate |
2005 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09541020_v17_n2_p163_Mataloni https://hdl.handle.net/20.500.12110/paper_09541020_v17_n2_p163_Mataloni |
long_lat |
ENVELOPE(-60.873,-60.873,-64.156,-64.156) ENVELOPE(-60.883,-60.883,-64.150,-64.150) ENVELOPE(-60.967,-60.967,-64.150,-64.150) ENVELOPE(-61.033,-61.033,-64.717,-64.717) ENVELOPE(-62.000,-62.000,-64.700,-64.700) ENVELOPE(-60.800,-60.800,-62.450,-62.450) |
geographic |
Antarctic Antarctic Peninsula Arctic Argentina Cierva Cierva Cove Cierva Point Danco Danco Coast Pingüinera West Antarctica |
geographic_facet |
Antarctic Antarctic Peninsula Arctic Argentina Cierva Cierva Cove Cierva Point Danco Danco Coast Pingüinera West Antarctica |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctica Arctic West Antarctica |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctica Arctic West Antarctica |
op_relation |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09541020_v17_n2_p163_Mataloni http://hdl.handle.net/20.500.12110/paper_09541020_v17_n2_p163_Mataloni |
op_doi |
https://doi.org/20.500.12110/paper_09541020_v17_n2_p163_Mataloni |
_version_ |
1766255265188937728 |