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dc.contributor.authorPatrichka Wei-Yi Chen
dc.contributor.authorMadeline Olivia
dc.contributor.authorGwo-Ching Gong
dc.contributor.authorSen Jan
dc.contributor.authorAn-Yi Tsai
dc.contributor.otherInstitute of Marine Environment and Ecology, National Taiwan Ocean University, Keelung 202-24, Taiwan
dc.contributor.otherInstitute of Marine Environment and Ecology, National Taiwan Ocean University, Keelung 202-24, Taiwan
dc.contributor.otherInstitute of Marine Environment and Ecology, National Taiwan Ocean University, Keelung 202-24, Taiwan
dc.contributor.otherInstitute of Oceanography, National Taiwan University, Taipei 106319, Taiwan
dc.contributor.otherInstitute of Marine Environment and Ecology, National Taiwan Ocean University, Keelung 202-24, Taiwan
dc.date.accessioned2024-06-26T15:38:57Z
dc.date.accessioned2025-10-08T08:24:19Z
dc.date.available2025-10-08T08:24:19Z
dc.date.issued01-06-2024
dc.identifier.urihttp://digilib.fisipol.ugm.ac.id/repo/handle/15717717/35779
dc.description.abstractIn mesoscale eddies, the chemical properties and biological composition are different from those in the surrounding water due to their unique physical processes. The mechanism of physical–biological coupling in warm-core eddies is unclear, especially because no studies have examined the effects of environmental factors on bacteria and viruses. The purpose of the present study was to examine the influence of an anticyclonic warm eddy on the relationship between bacterial and viral abundances, as well as viral activity (viral production), at different depths. At the core of the warm eddy, the bacterial abundance (0.48 to 2.82 × 10<sup>5</sup> cells mL<sup>−1</sup>) fluctuated less than that outside the eddy (1.12 to 7.03 × 10<sup>5</sup> cells mL<sup>−1</sup>). In particular, there was a four-fold higher viral–bacterial abundance ratio (VBR) estimated within the eddy, below the layer of the deep chlorophyll maximum, than outside the eddy. An anticyclonic warm eddy with downwelling at its center may contribute to viruses being transmitted directly into the deep ocean through adsorption on particulate organic matter while sinking. Overall, our findings provide valuable insights into the interaction between bacterial and viral abundances and their ecological mechanisms within a warm eddy.
dc.language.isoEN
dc.publisherMDPI AG
dc.subject.lccMicrobiology
dc.titleViral Dynamics in the Tropical Pacific Ocean: A Comparison between Within and Outside a Warm Eddy
dc.typeArticle
dc.description.keywordswarm-core eddies
dc.description.keywordsbacteria
dc.description.keywordsviruses
dc.description.keywordsviral–bacterial abundance ratio
dc.description.keywordsdownwelling
dc.description.doi10.3390/v16060937
dc.title.journalViruses
dc.identifier.e-issn1999-4915
dc.identifier.oai8d422791d57247ddb72384ea807a9841
dc.journal.infoVolume 16, Issue 6


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