Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | 김성한 | - |
dc.date.accessioned | 2018-03-19T05:33:27Z | - |
dc.date.available | 2018-03-19T05:33:27Z | - |
dc.date.issued | 2016-01 | - |
dc.identifier.citation | DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, v. 123, Page. 102-112 | en_US |
dc.identifier.issn | 0967-0645 | - |
dc.identifier.issn | 1879-0100 | - |
dc.identifier.uri | https://www.sciencedirect.com/science/article/pii/S0967064515003239 | - |
dc.identifier.uri | http://hdl.handle.net/20.500.11754/48928 | - |
dc.description.abstract | We investigated the heterotrophic bacterial biomass and production in February 2012, in four habitats (a polynya, sea-ice zone, ice shelf, and the open sea) in the Amundsen Sea to determine the spatial distribution, controlling factors, and ecological role of the bacteria during a late phytoplankton bloom by Phaeocystis antarctica. Bacterial abundance (BA) and production (BP) were highest at the center of the polynya, and both were significantly correlated with phytoplankton biomass. BP accounted for average 17% of the organic carbon produced by phytoplankton primary production (PP), which is higher than the average BP:PP ratio reported in most open ocean. The abundance of heterotrophic nanoflagellates (HNF) was correlated with the BA, and the average bacteria:HNF ratio (260) was lower than the values reported in most marine environments (400-1000), including the Ross Sea Polynya (800). Evidence for a tight coupling of bacteria and phytoplanlcton activities on the one hand and intense HNF grazing on bacteria on the other could be found in the high BP:PP and low bacteria:HNF ratios, respectively. Interestingly, these data were accompanied by low particulate carbon export fluxes measured during the late Phaeocystis bloom. Together, these results indicated that the microbial loop plays a significant role in the bio-geochemical carbon cycle and food web processes in the Amundsen Sea Polynya. (C) 2015 Elsevier Ltd. All rights reserved. | en_US |
dc.description.sponsorship | We thank the captain and crew of the Korean Research Icebreaker, Araon, for their assistance, and Dr. T.W. Kim for providing the site map. We also thank Prof. H.W. Ducklow and two reviewers for their valuable comments that improved the earlier version of the manuscript. This research was funded by the Korea Polar Research Institute (PP15020). | en_US |
dc.language.iso | en_US | en_US |
dc.publisher | PERGAMON-ELSEVIER SCIENCE LTD | en_US |
dc.subject | Bacterial production | en_US |
dc.subject | Microbial loop | en_US |
dc.subject | Amundsen Sea | en_US |
dc.subject | Polynya | en_US |
dc.subject | Phaeocystis bloom | en_US |
dc.subject | DISSOLVED ORGANIC-MATTER | en_US |
dc.subject | MICROBIAL FOOD-WEB | en_US |
dc.subject | MELTING GLACIERS FUELS | en_US |
dc.subject | PINE ISLAND GLACIER | en_US |
dc.subject | SOUTHERN-OCEAN | en_US |
dc.subject | ROSS SEA | en_US |
dc.subject | COASTAL WATERS | en_US |
dc.subject | SPRING BLOOM | en_US |
dc.subject | EUPHAUSIA-CRYSTALLOROPHIAS | en_US |
dc.subject | PHAEOCYSTIS-ANTARCTICA | en_US |
dc.title | Biomass, production, and control of heterotrophic bacterioplankton during a late phytoplankton bloom in the Amundsen Sea Polynya, Antarctica | en_US |
dc.type | Article | en_US |
dc.relation.volume | 123 | - |
dc.identifier.doi | 10.1016/j.dsr2.2015.10.001 | - |
dc.relation.page | 102-112 | - |
dc.relation.journal | DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY | - |
dc.contributor.googleauthor | Hyun, Jung-Ho | - |
dc.contributor.googleauthor | Kim, Sung-Han | - |
dc.contributor.googleauthor | Yang, Eun Jin | - |
dc.contributor.googleauthor | Choi, Ayeon | - |
dc.contributor.googleauthor | Lee, Sang Hoon | - |
dc.relation.code | 2016000426 | - |
dc.sector.campus | E | - |
dc.sector.daehak | RESEARCH INSTITUTE[E] | - |
dc.sector.department | INSTITUTE OF OCENA AND ATMOSPHERIC SCIENCES | - |
dc.identifier.pid | shkim1778 | - |
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