2010
DOI: 10.1007/s00300-010-0798-8
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Effect of ice melting on bacterial carbon fluxes channelled by viruses and protists in the Arctic Ocean

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Cited by 62 publications
(40 citation statements)
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“…Viral lysates are rich in free and combined amino acids (Middelboe & Jørgensen 2006), and bacterial mineralization of these compounds is associated with the production of ammonium (e.g. Hollibaugh 1978, Haaber & Middelboe 2009, Boras et al 2010. In turn, viral-induced ammonium regeneration resulted in increased growth of phytoplankton, thus implying that viral infection is an important mechanism in N recycling in the sea.…”
Section: Discussionmentioning
confidence: 99%
“…Viral lysates are rich in free and combined amino acids (Middelboe & Jørgensen 2006), and bacterial mineralization of these compounds is associated with the production of ammonium (e.g. Hollibaugh 1978, Haaber & Middelboe 2009, Boras et al 2010. In turn, viral-induced ammonium regeneration resulted in increased growth of phytoplankton, thus implying that viral infection is an important mechanism in N recycling in the sea.…”
Section: Discussionmentioning
confidence: 99%
“…90 % of standing stock lysed d −1 vs. 23 % d −1 , whereas grazing by heterotrophic nanoflagellates accounted for about one third of the mortality of the standing stock (W. Weinbauer, personal communication, 2012). The estimated burst size was on average 7 viruses per lysed bacterium cell (estimated from the net loss of HP and net production of viruses), which may seem somewhat low (see review by Parada et al, 2006), but Middelboe et al (2002) have observed similar burst sizes in Arctic water during summer and Boras et al (2010) have reported a burst size of 1-59 viruses per bacterium in north Svalbard during summer. Interestingly, specifically the HDNA HP were affected.…”
Section: Phasementioning
confidence: 99%
“…Significantly more carbon was channeled to protists in waters affected by ice melting than in unaffected waters. However, release of DOM due to viral lysis was also suppressed in receiving ice melt waters (Boras et al, 2010). These results indicated that sea ice melting in the Arctic could impact the carbon flow through the microbial food web.…”
Section: Microbial Plankton During the Arctic Winter -Carlos Pedrós-amentioning
confidence: 70%
“…The consequences of these increasing temperatures are already evident in the Arctic; for example, the loss of ice coverage is now affecting the habitat of large mammals, birds and humans (Duarte et al, 2012;Smetacek and Nicol, 2005). Also, extensive sea ice melting has led to major changes in the biogeochemistry (Chen et al, 2003;Wassmann et al, 2011) of the Arctic Ocean and in the functioning of microbial food webs (Boras et al, 2010). However, most research has focused on the summer period, and there are still few annual or over-winter microplankton data for the Arctic (Forest et al, 2011;Vaqué et al, 2008) or Antarctic (Kang et al, 2002) Oceans to confirm these changes and to build carbon flux models (Danovaro et al, 2011) to help understand the role of microplankton in this changing scenario.…”
Section: Microbial Plankton During the Arctic Winter -Carlos Pedrós-amentioning
confidence: 99%
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