Seawater carbonate chemistry, virioplankton and bacterioplankton in a shallow CO2-dominated hydrothermal vent (Panarea Island, Tyrrhenian Sea)

Gas hydrothermal vents are used as a natural analogue for studying the effects of CO2 leakage from hypothetical shallow marine storage sites on benthic and pelagic systems. This study investigated the interrelationships between planktonic prokaryotes and viruses in the Panarea Islands hydrothermal s...

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Main Authors: Karuza, Ana, Celussi, Mauro, Cibic, Tamara, Del Negro, Paola, De Vittor, Cinzia
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.778196
https://doi.org/10.1594/PANGAEA.778196
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.778196
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.778196 2024-09-15T18:28:06+00:00 Seawater carbonate chemistry, virioplankton and bacterioplankton in a shallow CO2-dominated hydrothermal vent (Panarea Island, Tyrrhenian Sea) Karuza, Ana Celussi, Mauro Cibic, Tamara Del Negro, Paola De Vittor, Cinzia MEDIAN LATITUDE: 38.634024 * MEDIAN LONGITUDE: 15.100829 * SOUTH-BOUND LATITUDE: 38.633611 * WEST-BOUND LONGITUDE: 15.100278 * NORTH-BOUND LATITUDE: 38.634444 * EAST-BOUND LONGITUDE: 15.101389 * MINIMUM DEPTH, water: 0.5 m * MAXIMUM DEPTH, water: 24.5 m 2012 text/tab-separated-values, 4444 data points https://doi.pangaea.de/10.1594/PANGAEA.778196 https://doi.org/10.1594/PANGAEA.778196 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.778196 https://doi.org/10.1594/PANGAEA.778196 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Karuza, Ana; Celussi, Mauro; Cibic, Tamara; Del Negro, Paola; De Vittor, Cinzia (2012): Virioplankton and bacterioplankton in a shallow CO2-dominated hydrothermal vent (Panarea Island, Tyrrhenian Sea). Estuarine, Coastal and Shelf Science, 97, 10-18, https://doi.org/10.1016/j.ecss.2011.10.027 Alkalinity total Aragonite saturation state Bicarbonate ion Biomass/Abundance/Elemental composition Calcite saturation state Calculated see reference(s) Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved organic Carbonate ion Carbonate system computation flag Carbon dioxide CO2 vent Coast and continental shelf Community composition and diversity Density DEPTH water Entire community Epifluorescence microscopy EPOCA EUR-OCEANS European network of excellence for Ocean Ecosystems Analysis European Project on Ocean Acidification Field observation Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Identification Infrared spectroscopy LATITUDE LONGITUDE Mediterranean Sea OA-ICC Ocean Acidification International Coordination Centre Oxygen saturation Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Prokaryotes standard deviation Salinity dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.77819610.1016/j.ecss.2011.10.027 2024-07-24T02:31:31Z Gas hydrothermal vents are used as a natural analogue for studying the effects of CO2 leakage from hypothetical shallow marine storage sites on benthic and pelagic systems. This study investigated the interrelationships between planktonic prokaryotes and viruses in the Panarea Islands hydrothermal system (southern Tyrrhenian Sea, Italy), especially their abundance, distribution and diversity. No difference in prokaryotic abundance was shown between high-CO2 and control sites. The community structure displayed differences between fumarolic field and the control, and between surface and bottom waters, the latter likely due to the presence of different water masses. Bacterial assemblages were qualitatively dominated by chemo- and photoautotrophic organisms, able to utilise both CO2 and H2S for their metabolic requirements. From significantly lower virioplankton abundance in the proximity of the exhalative area together with particularly low Virus-to-Prokaryotes Ratio, we inferred a reduced impact on prokaryotic abundance and proliferation. Even if the fate of viruses in this particular condition remains still unknown, we consider that lower viral abundance could reflect in enhancing the energy flow to higher trophic levels, thus largely influencing the overall functioning of the system. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(15.100278,15.101389,38.634444,38.633611)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Alkalinity
total
Aragonite saturation state
Bicarbonate ion
Biomass/Abundance/Elemental composition
Calcite saturation state
Calculated
see reference(s)
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
organic
Carbonate ion
Carbonate system computation flag
Carbon dioxide
CO2 vent
Coast and continental shelf
Community composition and diversity
Density
DEPTH
water
Entire community
Epifluorescence microscopy
EPOCA
EUR-OCEANS
European network of excellence for Ocean Ecosystems Analysis
European Project on Ocean Acidification
Field observation
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Identification
Infrared spectroscopy
LATITUDE
LONGITUDE
Mediterranean Sea
OA-ICC
Ocean Acidification International Coordination Centre
Oxygen saturation
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
pH
Prokaryotes
standard deviation
Salinity
spellingShingle Alkalinity
total
Aragonite saturation state
Bicarbonate ion
Biomass/Abundance/Elemental composition
Calcite saturation state
Calculated
see reference(s)
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
organic
Carbonate ion
Carbonate system computation flag
Carbon dioxide
CO2 vent
Coast and continental shelf
Community composition and diversity
Density
DEPTH
water
Entire community
Epifluorescence microscopy
EPOCA
EUR-OCEANS
European network of excellence for Ocean Ecosystems Analysis
European Project on Ocean Acidification
Field observation
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Identification
Infrared spectroscopy
LATITUDE
LONGITUDE
Mediterranean Sea
OA-ICC
Ocean Acidification International Coordination Centre
Oxygen saturation
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
pH
Prokaryotes
standard deviation
Salinity
Karuza, Ana
Celussi, Mauro
Cibic, Tamara
Del Negro, Paola
De Vittor, Cinzia
Seawater carbonate chemistry, virioplankton and bacterioplankton in a shallow CO2-dominated hydrothermal vent (Panarea Island, Tyrrhenian Sea)
topic_facet Alkalinity
total
Aragonite saturation state
Bicarbonate ion
Biomass/Abundance/Elemental composition
Calcite saturation state
Calculated
see reference(s)
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
organic
Carbonate ion
Carbonate system computation flag
Carbon dioxide
CO2 vent
Coast and continental shelf
Community composition and diversity
Density
DEPTH
water
Entire community
Epifluorescence microscopy
EPOCA
EUR-OCEANS
European network of excellence for Ocean Ecosystems Analysis
European Project on Ocean Acidification
Field observation
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Identification
Infrared spectroscopy
LATITUDE
LONGITUDE
Mediterranean Sea
OA-ICC
Ocean Acidification International Coordination Centre
Oxygen saturation
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
pH
Prokaryotes
standard deviation
Salinity
description Gas hydrothermal vents are used as a natural analogue for studying the effects of CO2 leakage from hypothetical shallow marine storage sites on benthic and pelagic systems. This study investigated the interrelationships between planktonic prokaryotes and viruses in the Panarea Islands hydrothermal system (southern Tyrrhenian Sea, Italy), especially their abundance, distribution and diversity. No difference in prokaryotic abundance was shown between high-CO2 and control sites. The community structure displayed differences between fumarolic field and the control, and between surface and bottom waters, the latter likely due to the presence of different water masses. Bacterial assemblages were qualitatively dominated by chemo- and photoautotrophic organisms, able to utilise both CO2 and H2S for their metabolic requirements. From significantly lower virioplankton abundance in the proximity of the exhalative area together with particularly low Virus-to-Prokaryotes Ratio, we inferred a reduced impact on prokaryotic abundance and proliferation. Even if the fate of viruses in this particular condition remains still unknown, we consider that lower viral abundance could reflect in enhancing the energy flow to higher trophic levels, thus largely influencing the overall functioning of the system.
format Dataset
author Karuza, Ana
Celussi, Mauro
Cibic, Tamara
Del Negro, Paola
De Vittor, Cinzia
author_facet Karuza, Ana
Celussi, Mauro
Cibic, Tamara
Del Negro, Paola
De Vittor, Cinzia
author_sort Karuza, Ana
title Seawater carbonate chemistry, virioplankton and bacterioplankton in a shallow CO2-dominated hydrothermal vent (Panarea Island, Tyrrhenian Sea)
title_short Seawater carbonate chemistry, virioplankton and bacterioplankton in a shallow CO2-dominated hydrothermal vent (Panarea Island, Tyrrhenian Sea)
title_full Seawater carbonate chemistry, virioplankton and bacterioplankton in a shallow CO2-dominated hydrothermal vent (Panarea Island, Tyrrhenian Sea)
title_fullStr Seawater carbonate chemistry, virioplankton and bacterioplankton in a shallow CO2-dominated hydrothermal vent (Panarea Island, Tyrrhenian Sea)
title_full_unstemmed Seawater carbonate chemistry, virioplankton and bacterioplankton in a shallow CO2-dominated hydrothermal vent (Panarea Island, Tyrrhenian Sea)
title_sort seawater carbonate chemistry, virioplankton and bacterioplankton in a shallow co2-dominated hydrothermal vent (panarea island, tyrrhenian sea)
publisher PANGAEA
publishDate 2012
url https://doi.pangaea.de/10.1594/PANGAEA.778196
https://doi.org/10.1594/PANGAEA.778196
op_coverage MEDIAN LATITUDE: 38.634024 * MEDIAN LONGITUDE: 15.100829 * SOUTH-BOUND LATITUDE: 38.633611 * WEST-BOUND LONGITUDE: 15.100278 * NORTH-BOUND LATITUDE: 38.634444 * EAST-BOUND LONGITUDE: 15.101389 * MINIMUM DEPTH, water: 0.5 m * MAXIMUM DEPTH, water: 24.5 m
long_lat ENVELOPE(15.100278,15.101389,38.634444,38.633611)
genre Ocean acidification
genre_facet Ocean acidification
op_source Supplement to: Karuza, Ana; Celussi, Mauro; Cibic, Tamara; Del Negro, Paola; De Vittor, Cinzia (2012): Virioplankton and bacterioplankton in a shallow CO2-dominated hydrothermal vent (Panarea Island, Tyrrhenian Sea). Estuarine, Coastal and Shelf Science, 97, 10-18, https://doi.org/10.1016/j.ecss.2011.10.027
op_relation https://doi.pangaea.de/10.1594/PANGAEA.778196
https://doi.org/10.1594/PANGAEA.778196
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.77819610.1016/j.ecss.2011.10.027
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