Growth rate over time of Emiliania huxleyi during laboratory experiments

Emiliania huxleyi was incubated for two years (2015-11-20 to 2017-12-01) under two conditions: present-day subantarctic water during summer (11°C and pH 8.1; Now), and projected conditions for subantarctic water by 2100 (14°C and pH 7.8; Future; Law et al. 2018). The pH was reduced by 0.3 units by b...

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Main Authors: Armstrong, Evelyn, Law, Cliff S
Format: Dataset
Language:English
Published: PANGAEA 2023
Subjects:
NIS
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.959829
https://doi.org/10.1594/PANGAEA.959829
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.959829
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.959829 2024-10-13T14:10:02+00:00 Growth rate over time of Emiliania huxleyi during laboratory experiments Armstrong, Evelyn Law, Cliff S LATITUDE: -45.829000 * LONGITUDE: 171.532000 * DATE/TIME START: 2014-06-03T00:00:00 * DATE/TIME END: 2014-06-03T00:00:00 2023 text/tab-separated-values, 670 data points https://doi.pangaea.de/10.1594/PANGAEA.959829 https://doi.org/10.1594/PANGAEA.959829 en eng PANGAEA https://doi.org/10.1594/PANGAEA.959857 Armstrong, Evelyn; Law, Cliff S (2023): Resilience of Emiliania huxleyi to future changes in subantarctic waters. PLoS ONE, 18(11), e0284415, https://doi.org/10.1371/journal.pone.0284415 DOE (1994): Handbook of methods for the analysis of the various parameters of the carbon dioxide system in sea water, version 2. A. G. Dickson & C. Goyet, eds., 187 pp, hdl:10013/epic.51788.d001 Law, Cliff S; Rickard, Graham J; Mikaloff Fletcher, Sara E; Pinkerton, Matt; Behrens, Erik; Chiswell, Stephen M; Currie, Kim (2018): Climate change projections for the surface ocean around New Zealand. New Zealand Journal of Marine and Freshwater Research, 52(3), 309-335, https://doi.org/10.1080/00288330.2017.1390772 Strzepek, Robert F; Maldonado, Maria T; Hunter, Keith A; Frew, Russell D; Boyd, Philip W (2011): Adaptive strategies by Southern Ocean phytoplankton to lessen iron limitation: Uptake of organically complexed iron and reduced cellular iron requirements. Limnology and Oceanography, 56(6), 1983-2002, https://doi.org/10.4319/lo.2011.56.6.1983 https://doi.pangaea.de/10.1594/PANGAEA.959829 https://doi.org/10.1594/PANGAEA.959829 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess adaptation Bottle Niskin Emiliania_huxleyi_subantarctic Emiliania huxleyi growth rate Fluorometer Turner Designs 10-AU Laboratory experiment NIS Ocean acidification ocean warming P140603 Polaris II Species unique identification unique identification (Semantic URI) unique identification (URI) subantarctic Time in days Treatment Type of study dataset 2023 ftpangaea https://doi.org/10.1594/PANGAEA.95982910.1594/PANGAEA.95985710.1371/journal.pone.028441510.1080/00288330.2017.139077210.4319/lo.2011.56.6.1983 2024-09-18T00:10:44Z Emiliania huxleyi was incubated for two years (2015-11-20 to 2017-12-01) under two conditions: present-day subantarctic water during summer (11°C and pH 8.1; Now), and projected conditions for subantarctic water by 2100 (14°C and pH 7.8; Future; Law et al. 2018). The pH was reduced by 0.3 units by bubbling 10% CO₂ through the medium prior to the addition of coccolithophore cells and confirmed using a spectrophotometric method (DOE 1994). One culture of each treatment was maintained in a semi-batch style to ensure the cells remained in exponential growth, with cell concentration maintained at low levels (<80000 cells ml⁻¹) to maintain pH at the target value. The pH of the medium after cell growth was checked periodically using a spectrophotometric method (DOE 1994) and was always found to be at the target pH. The in vivo fluorescence of the cultures was measured with a Turner 10-AU fluorometer and the growth rate of the cultures was calculated from the least squares regression of the natural logarithm of in vivo fluorescence, versus time during exponential growth (Strzepek et al. 2011). Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(171.532000,171.532000,-45.829000,-45.829000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic adaptation
Bottle
Niskin
Emiliania_huxleyi_subantarctic
Emiliania huxleyi
growth rate
Fluorometer
Turner Designs
10-AU
Laboratory experiment
NIS
Ocean acidification
ocean warming
P140603
Polaris II
Species
unique identification
unique identification (Semantic URI)
unique identification (URI)
subantarctic
Time in days
Treatment
Type of study
spellingShingle adaptation
Bottle
Niskin
Emiliania_huxleyi_subantarctic
Emiliania huxleyi
growth rate
Fluorometer
Turner Designs
10-AU
Laboratory experiment
NIS
Ocean acidification
ocean warming
P140603
Polaris II
Species
unique identification
unique identification (Semantic URI)
unique identification (URI)
subantarctic
Time in days
Treatment
Type of study
Armstrong, Evelyn
Law, Cliff S
Growth rate over time of Emiliania huxleyi during laboratory experiments
topic_facet adaptation
Bottle
Niskin
Emiliania_huxleyi_subantarctic
Emiliania huxleyi
growth rate
Fluorometer
Turner Designs
10-AU
Laboratory experiment
NIS
Ocean acidification
ocean warming
P140603
Polaris II
Species
unique identification
unique identification (Semantic URI)
unique identification (URI)
subantarctic
Time in days
Treatment
Type of study
description Emiliania huxleyi was incubated for two years (2015-11-20 to 2017-12-01) under two conditions: present-day subantarctic water during summer (11°C and pH 8.1; Now), and projected conditions for subantarctic water by 2100 (14°C and pH 7.8; Future; Law et al. 2018). The pH was reduced by 0.3 units by bubbling 10% CO₂ through the medium prior to the addition of coccolithophore cells and confirmed using a spectrophotometric method (DOE 1994). One culture of each treatment was maintained in a semi-batch style to ensure the cells remained in exponential growth, with cell concentration maintained at low levels (<80000 cells ml⁻¹) to maintain pH at the target value. The pH of the medium after cell growth was checked periodically using a spectrophotometric method (DOE 1994) and was always found to be at the target pH. The in vivo fluorescence of the cultures was measured with a Turner 10-AU fluorometer and the growth rate of the cultures was calculated from the least squares regression of the natural logarithm of in vivo fluorescence, versus time during exponential growth (Strzepek et al. 2011).
format Dataset
author Armstrong, Evelyn
Law, Cliff S
author_facet Armstrong, Evelyn
Law, Cliff S
author_sort Armstrong, Evelyn
title Growth rate over time of Emiliania huxleyi during laboratory experiments
title_short Growth rate over time of Emiliania huxleyi during laboratory experiments
title_full Growth rate over time of Emiliania huxleyi during laboratory experiments
title_fullStr Growth rate over time of Emiliania huxleyi during laboratory experiments
title_full_unstemmed Growth rate over time of Emiliania huxleyi during laboratory experiments
title_sort growth rate over time of emiliania huxleyi during laboratory experiments
publisher PANGAEA
publishDate 2023
url https://doi.pangaea.de/10.1594/PANGAEA.959829
https://doi.org/10.1594/PANGAEA.959829
op_coverage LATITUDE: -45.829000 * LONGITUDE: 171.532000 * DATE/TIME START: 2014-06-03T00:00:00 * DATE/TIME END: 2014-06-03T00:00:00
long_lat ENVELOPE(171.532000,171.532000,-45.829000,-45.829000)
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://doi.org/10.1594/PANGAEA.959857
Armstrong, Evelyn; Law, Cliff S (2023): Resilience of Emiliania huxleyi to future changes in subantarctic waters. PLoS ONE, 18(11), e0284415, https://doi.org/10.1371/journal.pone.0284415
DOE (1994): Handbook of methods for the analysis of the various parameters of the carbon dioxide system in sea water, version 2. A. G. Dickson & C. Goyet, eds., 187 pp, hdl:10013/epic.51788.d001
Law, Cliff S; Rickard, Graham J; Mikaloff Fletcher, Sara E; Pinkerton, Matt; Behrens, Erik; Chiswell, Stephen M; Currie, Kim (2018): Climate change projections for the surface ocean around New Zealand. New Zealand Journal of Marine and Freshwater Research, 52(3), 309-335, https://doi.org/10.1080/00288330.2017.1390772
Strzepek, Robert F; Maldonado, Maria T; Hunter, Keith A; Frew, Russell D; Boyd, Philip W (2011): Adaptive strategies by Southern Ocean phytoplankton to lessen iron limitation: Uptake of organically complexed iron and reduced cellular iron requirements. Limnology and Oceanography, 56(6), 1983-2002, https://doi.org/10.4319/lo.2011.56.6.1983
https://doi.pangaea.de/10.1594/PANGAEA.959829
https://doi.org/10.1594/PANGAEA.959829
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.95982910.1594/PANGAEA.95985710.1371/journal.pone.028441510.1080/00288330.2017.139077210.4319/lo.2011.56.6.1983
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