Edmonson Point (EP) in the Northern Victoria Land is a volcanic area close to Mt. Melbourne. It is characterized by alluvial sediments and weathered basaltic outcrops with some ponds and not far penguin rookeries. Here, soils are quite rich in organic content (0.5-1.6 % C org) and are Aquic Haplorthels overlying continuous permafrost. Permafrost soil samples were collected directly from the unfrozen part (35 cm in depth) of the active layer at EP in early January 2014. Temperature was measured from surface to 35 cm (just above the permafrost table), ranging from 7.4 to 1.8°C. Samples were examined for: bacterial community composition by the Ion Torrent (IT) technique, prokaryotic abundance and cell-shape by microscopic image-analysis (IA), viability by Live/Dead (L/D) stain, respiring cell quantification by 5-Cyano-2,3-ditolyl-tetrazolium chloride (CTC+) stain, potential ectoenzymatic activities rates on proteins, polysaccharides and organic phosphates (by leucine-aminopeptidase, ß-glucosidase and alkaline-phosphatase, respectively), physiological profiles by Biolog-Ecoplate(TM), sub-population assessment according to nucleic acid contents by flow-cytometry (FC). Finally, different isolation procedures were adopted to recover aerobic bacteria and a selection of bacterial isolates was identified by the 16S rRNA gene sequencing.

Prokaryotic communites in permafrost soil at Edmonson Point (Northern Victoria Land).

Papale M;Lo Giudice A;Azzaro M;La Ferla R;Caruso G;Maimone G;
2016

Abstract

Edmonson Point (EP) in the Northern Victoria Land is a volcanic area close to Mt. Melbourne. It is characterized by alluvial sediments and weathered basaltic outcrops with some ponds and not far penguin rookeries. Here, soils are quite rich in organic content (0.5-1.6 % C org) and are Aquic Haplorthels overlying continuous permafrost. Permafrost soil samples were collected directly from the unfrozen part (35 cm in depth) of the active layer at EP in early January 2014. Temperature was measured from surface to 35 cm (just above the permafrost table), ranging from 7.4 to 1.8°C. Samples were examined for: bacterial community composition by the Ion Torrent (IT) technique, prokaryotic abundance and cell-shape by microscopic image-analysis (IA), viability by Live/Dead (L/D) stain, respiring cell quantification by 5-Cyano-2,3-ditolyl-tetrazolium chloride (CTC+) stain, potential ectoenzymatic activities rates on proteins, polysaccharides and organic phosphates (by leucine-aminopeptidase, ß-glucosidase and alkaline-phosphatase, respectively), physiological profiles by Biolog-Ecoplate(TM), sub-population assessment according to nucleic acid contents by flow-cytometry (FC). Finally, different isolation procedures were adopted to recover aerobic bacteria and a selection of bacterial isolates was identified by the 16S rRNA gene sequencing.
2016
Istituto per l'Ambiente Marino Costiero - IAMC - Sede Napoli
Inglese
Scientific Committee on Antarctic Research (SCAR) 2016 Open Science Conference
No
August 22-26, 2016
Kuala Lumpur, Malaysia
permafrost
prokaryotic community
antarctica
5
none
Papale M.; Conte A.; Michaud L.; Lo Giudice A.; Azzaro M.; La Ferla R.; Caruso G.; Maimone G.; Paranhos R.; Cabral A.S.; Rappazzo A.C.; Spanò N.; Gugl...espandi
273
info:eu-repo/semantics/conferenceObject
04 Contributo in convegno::04.01 Contributo in Atti di convegno
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/324373
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