Seawater carbonate chemistry and the physiological response variables of the high and ambient (i.e., control) CO2 mesocosms at different temperatures

Seagrass beds serve as important carbon sinks, and it is thought that increasing the quantity and quality of such sinks could help to slow the rate of global climate change. Therefore, it will be important to (1) gain a better understanding of seagrass bed metabolism and (2) document how these high-...

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Main Authors: Liu, Pi-Jen, Chang, Hong-Fong, Mayfield, Anderson B, Lin, Hsing-Juh
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.946381
https://doi.org/10.1594/PANGAEA.946381
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.946381
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.946381 2024-09-15T18:28:25+00:00 Seawater carbonate chemistry and the physiological response variables of the high and ambient (i.e., control) CO2 mesocosms at different temperatures Liu, Pi-Jen Chang, Hong-Fong Mayfield, Anderson B Lin, Hsing-Juh LATITUDE: 21.950000 * LONGITUDE: 120.730000 * DATE/TIME START: 2014-04-15T00:00:00 * DATE/TIME END: 2014-04-15T00:00:00 2022 text/tab-separated-values, 540 data points https://doi.pangaea.de/10.1594/PANGAEA.946381 https://doi.org/10.1594/PANGAEA.946381 en eng PANGAEA Liu, Pi-Jen; Chang, Hong-Fong; Mayfield, Anderson B; Lin, Hsing-Juh (2022): Assessing the Effects of Ocean Warming and Acidification on the Seagrass Thalassia hemprichii. Journal of Marine Science and Engineering, 10(6), 714, https://doi.org/10.3390/jmse10060714 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James (2021): seacarb: seawater carbonate chemistry with R. R package version 3.2.16. https://cran.r-project.org/web/packages/seacarb/index.html https://doi.pangaea.de/10.1594/PANGAEA.946381 https://doi.org/10.1594/PANGAEA.946381 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Alkalinity total standard deviation Ammonium Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Biomass dry mass Biomass/Abundance/Elemental composition Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved per shoot Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Carbon sequestration dataset 2022 ftpangaea https://doi.org/10.1594/PANGAEA.94638110.3390/jmse10060714 2024-07-24T02:31:34Z Seagrass beds serve as important carbon sinks, and it is thought that increasing the quantity and quality of such sinks could help to slow the rate of global climate change. Therefore, it will be important to (1) gain a better understanding of seagrass bed metabolism and (2) document how these high-productivity ecosystems are impacted by climate change-associated factors, such as ocean acidification (OA) and ocean warming (OW). A mesocosm-based approach was taken herein in which a tropical, Western Pacific seagrass species Thalassia hemprichii was cultured under either control or OA-simulating conditions; the temperature was gradually increased from 25 to 31 °C for both CO2 enrichment treatments, and it was hypothesized that this species would respond positively to OA and elevated temperature. After 12 weeks of exposure, OA (~1200 ppm) led to (1) increases in underground biomass and root C:N ratios and (2) decreases in root nitrogen content. Rising temperatures (25 to 31 °C) increased the maximum quantum yield of photosystem II (Fv:Fm), productivity, leaf growth rate, decomposition rate, and carbon sequestration, but decreased the rate of shoot density increase and the carbon content of the leaves; this indicates that warming alone does not increase the short-term carbon sink capacity of this seagrass species. Under high CO2 and the highest temperature employed (31 °C), this seagrass demonstrated its highest productivity, Fv:Fm, leaf growth rate, and carbon sequestration. Collectively, then, it appears that high CO2 levels offset the negative effects of high temperature on this seagrass species. Whether this pattern is maintained at temperatures that actually induce marked seagrass stress (likely beginning at 33–34 °C in Southern Taiwan) should be the focus of future research. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(120.730000,120.730000,21.950000,21.950000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Alkalinity
total
standard deviation
Ammonium
Animalia
Aragonite saturation state
Benthic animals
Benthos
Bicarbonate ion
Biomass
dry mass
Biomass/Abundance/Elemental composition
Calcite saturation state
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
per shoot
Carbon/Nitrogen ratio
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Carbon sequestration
spellingShingle Alkalinity
total
standard deviation
Ammonium
Animalia
Aragonite saturation state
Benthic animals
Benthos
Bicarbonate ion
Biomass
dry mass
Biomass/Abundance/Elemental composition
Calcite saturation state
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
per shoot
Carbon/Nitrogen ratio
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Carbon sequestration
Liu, Pi-Jen
Chang, Hong-Fong
Mayfield, Anderson B
Lin, Hsing-Juh
Seawater carbonate chemistry and the physiological response variables of the high and ambient (i.e., control) CO2 mesocosms at different temperatures
topic_facet Alkalinity
total
standard deviation
Ammonium
Animalia
Aragonite saturation state
Benthic animals
Benthos
Bicarbonate ion
Biomass
dry mass
Biomass/Abundance/Elemental composition
Calcite saturation state
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
per shoot
Carbon/Nitrogen ratio
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Carbon sequestration
description Seagrass beds serve as important carbon sinks, and it is thought that increasing the quantity and quality of such sinks could help to slow the rate of global climate change. Therefore, it will be important to (1) gain a better understanding of seagrass bed metabolism and (2) document how these high-productivity ecosystems are impacted by climate change-associated factors, such as ocean acidification (OA) and ocean warming (OW). A mesocosm-based approach was taken herein in which a tropical, Western Pacific seagrass species Thalassia hemprichii was cultured under either control or OA-simulating conditions; the temperature was gradually increased from 25 to 31 °C for both CO2 enrichment treatments, and it was hypothesized that this species would respond positively to OA and elevated temperature. After 12 weeks of exposure, OA (~1200 ppm) led to (1) increases in underground biomass and root C:N ratios and (2) decreases in root nitrogen content. Rising temperatures (25 to 31 °C) increased the maximum quantum yield of photosystem II (Fv:Fm), productivity, leaf growth rate, decomposition rate, and carbon sequestration, but decreased the rate of shoot density increase and the carbon content of the leaves; this indicates that warming alone does not increase the short-term carbon sink capacity of this seagrass species. Under high CO2 and the highest temperature employed (31 °C), this seagrass demonstrated its highest productivity, Fv:Fm, leaf growth rate, and carbon sequestration. Collectively, then, it appears that high CO2 levels offset the negative effects of high temperature on this seagrass species. Whether this pattern is maintained at temperatures that actually induce marked seagrass stress (likely beginning at 33–34 °C in Southern Taiwan) should be the focus of future research.
format Dataset
author Liu, Pi-Jen
Chang, Hong-Fong
Mayfield, Anderson B
Lin, Hsing-Juh
author_facet Liu, Pi-Jen
Chang, Hong-Fong
Mayfield, Anderson B
Lin, Hsing-Juh
author_sort Liu, Pi-Jen
title Seawater carbonate chemistry and the physiological response variables of the high and ambient (i.e., control) CO2 mesocosms at different temperatures
title_short Seawater carbonate chemistry and the physiological response variables of the high and ambient (i.e., control) CO2 mesocosms at different temperatures
title_full Seawater carbonate chemistry and the physiological response variables of the high and ambient (i.e., control) CO2 mesocosms at different temperatures
title_fullStr Seawater carbonate chemistry and the physiological response variables of the high and ambient (i.e., control) CO2 mesocosms at different temperatures
title_full_unstemmed Seawater carbonate chemistry and the physiological response variables of the high and ambient (i.e., control) CO2 mesocosms at different temperatures
title_sort seawater carbonate chemistry and the physiological response variables of the high and ambient (i.e., control) co2 mesocosms at different temperatures
publisher PANGAEA
publishDate 2022
url https://doi.pangaea.de/10.1594/PANGAEA.946381
https://doi.org/10.1594/PANGAEA.946381
op_coverage LATITUDE: 21.950000 * LONGITUDE: 120.730000 * DATE/TIME START: 2014-04-15T00:00:00 * DATE/TIME END: 2014-04-15T00:00:00
long_lat ENVELOPE(120.730000,120.730000,21.950000,21.950000)
genre Ocean acidification
genre_facet Ocean acidification
op_relation Liu, Pi-Jen; Chang, Hong-Fong; Mayfield, Anderson B; Lin, Hsing-Juh (2022): Assessing the Effects of Ocean Warming and Acidification on the Seagrass Thalassia hemprichii. Journal of Marine Science and Engineering, 10(6), 714, https://doi.org/10.3390/jmse10060714
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James (2021): seacarb: seawater carbonate chemistry with R. R package version 3.2.16. https://cran.r-project.org/web/packages/seacarb/index.html
https://doi.pangaea.de/10.1594/PANGAEA.946381
https://doi.org/10.1594/PANGAEA.946381
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.94638110.3390/jmse10060714
_version_ 1810469790521753600