File Download
Links for fulltext
(May Require Subscription)
- Publisher Website: 10.1007/s00300-010-0872-2
- Scopus: eid_2-s2.0-79551680486
- WOS: WOS:000287904600015
- Find via
Supplementary
- Citations:
- Appears in Collections:
Article: Distribution and abiotic influences on hypolithic microbial communities in an Antarctic Dry Valley
Title | Distribution and abiotic influences on hypolithic microbial communities in an Antarctic Dry Valley | ||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Authors | |||||||||||||||
Keywords | Antarctica Cryptic microbial communities Hypolithons Microniches Miers valley | ||||||||||||||
Issue Date | 2011 | ||||||||||||||
Publisher | Springer Verlag. The Journal's web site is located at http://link.springer.de/link/service/journals/00300/index.htm | ||||||||||||||
Citation | Polar Biology, 2011, v. 34 n. 2, p. 307-311 How to Cite? | ||||||||||||||
Abstract | The Miers Valley within the McMurdo Dry Valleys of Antarctica supports abundant quartz and marble substrates for hypolithons-microbial colonists on the underside of these translucent rocks. Three physically distinct hypolithic community types have been identified: cyanobacteria dominated (Type I), fungus dominated (Type II) or moss dominated (Type III). The distribution of the three types was mapped across much of the ~75 km 2 area of the upper Miers Valley and correlated this with the measurements of selected micro-environmental variables. Type I hypolithons were most common and occurred at all altitudes up to 824 m, whilst Type II and Type III hypolithons were less abundant and restricted to lower altitudes on the valley floor (<415 m and <257 m, respectively). Whilst all colonized quartz effectively filtered incident UVB irradiance, transmittance levels for UVA and PAR varied markedly and were significant in determining hypolith type. Notably, the Type I hypolithons occurred under rocks with a significantly lower transmittance of photosynthetically active radiation than Type II and III hypolithons. Altitude and aspect were also significant factors determining hypolith type, and a role for altitude-related abiotic variables in determining the distribution of Type I, II and III hypolithons is proposed. © 2010 The Author(s). | ||||||||||||||
Persistent Identifier | http://hdl.handle.net/10722/145036 | ||||||||||||||
ISSN | 2023 Impact Factor: 1.5 2023 SCImago Journal Rankings: 0.566 | ||||||||||||||
ISI Accession Number ID |
Funding Information: This research was undertaken under the auspices of the South African Antarctic Research Project, Australian Antarctic Division (ASAC 2355) and the Waikato University Antarctic Terrestrial Biology Research Program. We thank Irfan Jones and Brian Storey (Gateway Antarctica, Univ. of Canterbury, NZ) for preparing Fig. 1. The authors gratefully acknowledge funding from the National Research Foundation (SA), the Hong Kong Research Grants Council (7733/08MM), Antarctica New Zealand and the NZ Foundation for Research Science & Technology (Terrestrial Antarctic Biocomplexity Survey, nzTABS). | ||||||||||||||
References |
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Cowan, DA | en_HK |
dc.contributor.author | Pointing, SB | en_HK |
dc.contributor.author | Stevens, MI | en_HK |
dc.contributor.author | Craig Cary, S | en_HK |
dc.contributor.author | Stomeo, F | en_HK |
dc.contributor.author | Tuffin, IM | en_HK |
dc.date.accessioned | 2012-02-21T05:43:02Z | - |
dc.date.available | 2012-02-21T05:43:02Z | - |
dc.date.issued | 2011 | en_HK |
dc.identifier.citation | Polar Biology, 2011, v. 34 n. 2, p. 307-311 | en_HK |
dc.identifier.issn | 0722-4060 | en_HK |
dc.identifier.uri | http://hdl.handle.net/10722/145036 | - |
dc.description.abstract | The Miers Valley within the McMurdo Dry Valleys of Antarctica supports abundant quartz and marble substrates for hypolithons-microbial colonists on the underside of these translucent rocks. Three physically distinct hypolithic community types have been identified: cyanobacteria dominated (Type I), fungus dominated (Type II) or moss dominated (Type III). The distribution of the three types was mapped across much of the ~75 km 2 area of the upper Miers Valley and correlated this with the measurements of selected micro-environmental variables. Type I hypolithons were most common and occurred at all altitudes up to 824 m, whilst Type II and Type III hypolithons were less abundant and restricted to lower altitudes on the valley floor (<415 m and <257 m, respectively). Whilst all colonized quartz effectively filtered incident UVB irradiance, transmittance levels for UVA and PAR varied markedly and were significant in determining hypolith type. Notably, the Type I hypolithons occurred under rocks with a significantly lower transmittance of photosynthetically active radiation than Type II and III hypolithons. Altitude and aspect were also significant factors determining hypolith type, and a role for altitude-related abiotic variables in determining the distribution of Type I, II and III hypolithons is proposed. © 2010 The Author(s). | en_HK |
dc.language | eng | en_US |
dc.publisher | Springer Verlag. The Journal's web site is located at http://link.springer.de/link/service/journals/00300/index.htm | en_HK |
dc.relation.ispartof | Polar Biology | en_HK |
dc.rights | The Author(s) | en_US |
dc.rights | This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License. | en_US |
dc.subject | Antarctica | en_HK |
dc.subject | Cryptic microbial communities | en_HK |
dc.subject | Hypolithons | en_HK |
dc.subject | Microniches | en_HK |
dc.subject | Miers valley | en_HK |
dc.title | Distribution and abiotic influences on hypolithic microbial communities in an Antarctic Dry Valley | en_HK |
dc.type | Article | en_HK |
dc.identifier.openurl | http://library.hku.hk:4551/resserv?sid=springerlink&genre=article&atitle=Distribution and abiotic influences on hypolithic microbial communities in an Antarctic Dry Valley&title=Polar Biology&issn=07224060&date=2011-02-01&volume=34&issue=2& spage=307&authors=Don A. Cowan, Stephen B. Pointing, Mark I. Stevens, <i>et al.</i> | en_US |
dc.identifier.email | Pointing, SB: pointing@hkucc.hku.hk | en_HK |
dc.identifier.authority | Pointing, SB=rp00771 | en_HK |
dc.description.nature | published_or_final_version | en_US |
dc.identifier.doi | 10.1007/s00300-010-0872-2 | en_HK |
dc.identifier.scopus | eid_2-s2.0-79551680486 | en_HK |
dc.relation.references | http://www.scopus.com/mlt/select.url?eid=2-s2.0-79551680486&selection=ref&src=s&origin=recordpage | en_HK |
dc.identifier.volume | 34 | en_HK |
dc.identifier.issue | 2 | en_HK |
dc.identifier.spage | 307 | en_HK |
dc.identifier.epage | 311 | en_HK |
dc.identifier.eissn | 1432-2056 | en_US |
dc.identifier.isi | WOS:000287904600015 | - |
dc.publisher.place | Germany | en_HK |
dc.description.other | Springer Open Choice, 21 Feb 2012 | en_US |
dc.identifier.scopusauthorid | Cowan, DA=24425600900 | en_HK |
dc.identifier.scopusauthorid | Pointing, SB=6603986412 | en_HK |
dc.identifier.scopusauthorid | Stevens, MI=13606264200 | en_HK |
dc.identifier.scopusauthorid | Craig Cary, S=9240110000 | en_HK |
dc.identifier.scopusauthorid | Stomeo, F=24377175100 | en_HK |
dc.identifier.scopusauthorid | Tuffin, IM=36945566200 | en_HK |
dc.identifier.citeulike | 7770966 | - |
dc.identifier.issnl | 0722-4060 | - |