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| "author_email": null, | | "author_email": null, |
| "code": "7b.b.hc", | | "code": "7b.b.hc", |
| "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", |
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| firstname\":\"Tristan\",\"lastname\":\"Biggs\",\"affiliation\":\"Royal | | firstname\":\"Tristan\",\"lastname\":\"Biggs\",\"affiliation\":\"Royal |
| Netherlands Institute for Sea | | Netherlands Institute for Sea |
| stname\":\"Corina\",\"lastname\":\"Brussaard\",\"affiliation\":\"Royal | | stname\":\"Corina\",\"lastname\":\"Brussaard\",\"affiliation\":\"Royal |
| Netherlands Institute for Sea | | Netherlands Institute for Sea |
| name\":\"Jef\",\"lastname\":\"Huisman\",\"affiliation\":\"Universiteit | | name\":\"Jef\",\"lastname\":\"Huisman\",\"affiliation\":\"Universiteit |
| van | | van |
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| "dates": | | "dates": |
| 22:00:00.000Z\",\"type\":\"collected\",\"information\":\"Environmental | | 22:00:00.000Z\",\"type\":\"collected\",\"information\":\"Environmental |
| and biological time series | | and biological time series |
| T23:00:00.000Z\",\"type\":\"collected\",\"information\":\"Experimental | | T23:00:00.000Z\",\"type\":\"collected\",\"information\":\"Experimental |
| time period\"}]", | | time period\"}]", |
| "deposit_date": "2021-05-07", | | "deposit_date": "2021-05-07", |
| "depositor": "Tristan Biggs", | | "depositor": "Tristan Biggs", |
| "distribution_date": "2021-05-07", | | "distribution_date": "2021-05-07", |
| "distributor": "Research Data Management(NIOZ Royal Netherlands | | "distributor": "Research Data Management(NIOZ Royal Netherlands |
| Institute for Sea Research)", | | Institute for Sea Research)", |
| "doi_date_published": "2021-05-07", | | "doi_date_published": "2021-05-07", |
| "funding_references": "[{\"name\":\"Dutch Research Council | | "funding_references": "[{\"name\":\"Dutch Research Council |
| (NWO)\",\"awardnumber\":\"866.10.102\",\"awardtitle\":\"Antarctic | | (NWO)\",\"awardnumber\":\"866.10.102\",\"awardtitle\":\"Antarctic |
| phytoplankton in a changing world and its consequences for the lower | | phytoplankton in a changing world and its consequences for the lower |
| pelagic food web (Antphirco)\"}]", | | pelagic food web (Antphirco)\"}]", |
| "geographic_coverage": "[{\"place\":\"Ryder | | "geographic_coverage": "[{\"place\":\"Ryder |
| ,\"longitude_1\":\"\",\"latitude_2\":68.231,\"longitude_2\":67.572}]", | | ,\"longitude_1\":\"\",\"latitude_2\":68.231,\"longitude_2\":67.572}]", |
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| "metadata_created": "2024-10-22T11:43:18.032856", | | "metadata_created": "2024-10-22T11:43:18.032856", |
| n | "metadata_modified": "2024-10-22T16:56:38.937366", | n | "metadata_modified": "2024-10-22T16:56:39.476367", |
| "name": "7bbhc", | | "name": "7bbhc", |
| "notes": "Phytoplankton form the base of marine food webs and are a | | "notes": "Phytoplankton form the base of marine food webs and are a |
| primary means for carbon export in the Southern Ocean, a key area for | | primary means for carbon export in the Southern Ocean, a key area for |
| global pCO2 drawdown. Viral lysis and grazing have very different | | global pCO2 drawdown. Viral lysis and grazing have very different |
| effects on microbial community dynamics and carbon export, yet, very | | effects on microbial community dynamics and carbon export, yet, very |
| little is known about the relative magnitude and ecological impact of | | little is known about the relative magnitude and ecological impact of |
| viral lysis on natural phytoplankton communities, especially in | | viral lysis on natural phytoplankton communities, especially in |
| Antarctic waters. Here, we report on the temporal dynamics and | | Antarctic waters. Here, we report on the temporal dynamics and |
| relative importance of viral lysis rates, in comparison to grazing, | | relative importance of viral lysis rates, in comparison to grazing, |
| for Antarctic nano- and pico-sized phytoplankton of varied taxonomy | | for Antarctic nano- and pico-sized phytoplankton of varied taxonomy |
| and size over a full productive season. Our results show that viral | | and size over a full productive season. Our results show that viral |
| lysis was a major loss factor throughout the season, responsible for | | lysis was a major loss factor throughout the season, responsible for |
| roughly half (58%) of seasonal phytoplankton carbon losses. Viral | | roughly half (58%) of seasonal phytoplankton carbon losses. Viral |
| lysis appeared critically important for explaining temporal dynamics | | lysis appeared critically important for explaining temporal dynamics |
| and for obtaining a complete seasonal mass balance of Antarctic | | and for obtaining a complete seasonal mass balance of Antarctic |
| phytoplankton. Group-specific responses indicated a negative | | phytoplankton. Group-specific responses indicated a negative |
| correlation between grazing and viral losses in Phaeocystis and | | correlation between grazing and viral losses in Phaeocystis and |
| picoeukaryotes, while for other phytoplankton groups losses were more | | picoeukaryotes, while for other phytoplankton groups losses were more |
| evenly spread throughout the season. Cryptophyte mortality was | | evenly spread throughout the season. Cryptophyte mortality was |
| dominated by viral lysis, whereas small diatoms were mostly grazed. | | dominated by viral lysis, whereas small diatoms were mostly grazed. |
| n | Larger diatoms dominated algal carbon flow and a single \u2018lysis | n | Larger diatoms dominated algal carbon flow and a single ???lysis |
| event\u2019 directed > 100% of daily carbon production away from | | event??? directed > 100% of daily carbon production away from higher |
| higher trophic levels. This study highlights the need to consider | | trophic levels. This study highlights the need to consider viral lysis |
| viral lysis of key Antarctic phytoplankton for a better understanding | | of key Antarctic phytoplankton for a better understanding of microbial |
| of microbial community interactions and more accurate predictions of | | community interactions and more accurate predictions of organic matter |
| organic matter flux in this climate-sensitive region.", | | flux in this climate-sensitive region.", |
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