Viral impacts on bacterial communities in Arctic cryoconite

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Viral impacts on bacterial communities in Arctic cryoconite. / Bellas, Christopher M.; Anesio, Alexandre M.; Telling, Jon; Stibal, Marek; Tranter, Martyn; Davis, Sean.

In: Environmental Research Letters, Vol. 8, No. 4, 045021, 2013.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Bellas, CM, Anesio, AM, Telling, J, Stibal, M, Tranter, M & Davis, S 2013, 'Viral impacts on bacterial communities in Arctic cryoconite', Environmental Research Letters, vol. 8, no. 4, 045021. https://doi.org/10.1088/1748-9326/8/4/045021

APA

Bellas, C. M., Anesio, A. M., Telling, J., Stibal, M., Tranter, M., & Davis, S. (2013). Viral impacts on bacterial communities in Arctic cryoconite. Environmental Research Letters, 8(4), [045021]. https://doi.org/10.1088/1748-9326/8/4/045021

Vancouver

Bellas CM, Anesio AM, Telling J, Stibal M, Tranter M, Davis S. Viral impacts on bacterial communities in Arctic cryoconite. Environmental Research Letters. 2013;8(4). 045021. https://doi.org/10.1088/1748-9326/8/4/045021

Author

Bellas, Christopher M. ; Anesio, Alexandre M. ; Telling, Jon ; Stibal, Marek ; Tranter, Martyn ; Davis, Sean. / Viral impacts on bacterial communities in Arctic cryoconite. In: Environmental Research Letters. 2013 ; Vol. 8, No. 4.

Bibtex

@article{56b7134be8844d9a94ac70a5cf6d4c8d,
title = "Viral impacts on bacterial communities in Arctic cryoconite",
abstract = "The surfaces of glaciers are extreme ecosystems dominated by microbial communities. Viruses are found in abundance here, with a high frequency of bacteria displaying visible virus infection. In this study, viral and bacterial production was measured in Arctic cryoconite holes to address the control that viruses play in these highly truncated ecosystems. Mean bacterial carbon production in the sediments of cryoconite holes was found to be 57.8 +/- 12.9 ng C g(-1) dry wt. h(-1), which predicted a mean of 1.89-5.41 x 10(6) cells g(-1) dry wt. h(-1) based on a range of conversion factors. Relative to this, virus production was found to be high, up to 8.98 x 10(7) virus like particles g(-1) dry wt. h(-1) were produced, which is comparable to virus production in sediments around the globe. The virus burst size was assessed by transmission electron microscopy and found to be amongst the lowest recorded in the literature (mean 2.4). Hence, to account for the measured virus production, the viral induced bacterial mortality was calculated to be more than capable of accounting for the mortality of all bacterial production. The data presented here, therefore, suggests that viral induced mortality is a dominant process for the release and recycling of carbon and nutrients in supraglacial ecosystems.",
keywords = "virus, bacteriophage, cryoconite, glacier, DOM",
author = "Bellas, {Christopher M.} and Anesio, {Alexandre M.} and Jon Telling and Marek Stibal and Martyn Tranter and Sean Davis",
note = "CENPERMOA[2013]",
year = "2013",
doi = "10.1088/1748-9326/8/4/045021",
language = "English",
volume = "8",
journal = "Environmental Research Letters",
issn = "1748-9326",
publisher = "IOP Publishing",
number = "4",

}

RIS

TY - JOUR

T1 - Viral impacts on bacterial communities in Arctic cryoconite

AU - Bellas, Christopher M.

AU - Anesio, Alexandre M.

AU - Telling, Jon

AU - Stibal, Marek

AU - Tranter, Martyn

AU - Davis, Sean

N1 - CENPERMOA[2013]

PY - 2013

Y1 - 2013

N2 - The surfaces of glaciers are extreme ecosystems dominated by microbial communities. Viruses are found in abundance here, with a high frequency of bacteria displaying visible virus infection. In this study, viral and bacterial production was measured in Arctic cryoconite holes to address the control that viruses play in these highly truncated ecosystems. Mean bacterial carbon production in the sediments of cryoconite holes was found to be 57.8 +/- 12.9 ng C g(-1) dry wt. h(-1), which predicted a mean of 1.89-5.41 x 10(6) cells g(-1) dry wt. h(-1) based on a range of conversion factors. Relative to this, virus production was found to be high, up to 8.98 x 10(7) virus like particles g(-1) dry wt. h(-1) were produced, which is comparable to virus production in sediments around the globe. The virus burst size was assessed by transmission electron microscopy and found to be amongst the lowest recorded in the literature (mean 2.4). Hence, to account for the measured virus production, the viral induced bacterial mortality was calculated to be more than capable of accounting for the mortality of all bacterial production. The data presented here, therefore, suggests that viral induced mortality is a dominant process for the release and recycling of carbon and nutrients in supraglacial ecosystems.

AB - The surfaces of glaciers are extreme ecosystems dominated by microbial communities. Viruses are found in abundance here, with a high frequency of bacteria displaying visible virus infection. In this study, viral and bacterial production was measured in Arctic cryoconite holes to address the control that viruses play in these highly truncated ecosystems. Mean bacterial carbon production in the sediments of cryoconite holes was found to be 57.8 +/- 12.9 ng C g(-1) dry wt. h(-1), which predicted a mean of 1.89-5.41 x 10(6) cells g(-1) dry wt. h(-1) based on a range of conversion factors. Relative to this, virus production was found to be high, up to 8.98 x 10(7) virus like particles g(-1) dry wt. h(-1) were produced, which is comparable to virus production in sediments around the globe. The virus burst size was assessed by transmission electron microscopy and found to be amongst the lowest recorded in the literature (mean 2.4). Hence, to account for the measured virus production, the viral induced bacterial mortality was calculated to be more than capable of accounting for the mortality of all bacterial production. The data presented here, therefore, suggests that viral induced mortality is a dominant process for the release and recycling of carbon and nutrients in supraglacial ecosystems.

KW - virus

KW - bacteriophage

KW - cryoconite

KW - glacier

KW - DOM

U2 - 10.1088/1748-9326/8/4/045021

DO - 10.1088/1748-9326/8/4/045021

M3 - Journal article

VL - 8

JO - Environmental Research Letters

JF - Environmental Research Letters

SN - 1748-9326

IS - 4

M1 - 045021

ER -

ID: 119832012