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  • PANGAEA  (2)
  • 2015-2019  (2)
Publikationsart
Schlagwörter
Erscheinungszeitraum
Jahr
  • 1
    Publikationsdatum: 2024-01-09
    Beschreibung: This dataset contains measurements of δ11B, δ13C and δ18O, as well as the elemental ratios Magnesium/Calcium, Aluminium/Calcium, Strontium/Calcium from planktic foraminifera from six different ODP sites.
    Schlagwort(e): 114-702B; 143-865B; 143-865C; 207-1260A; 207-1260B; 208-1263B; AGE; Al/Ca; Aluminium/Calcium ratio; boron isotopes; Calculated; Depth, description; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Foraminifera, planktic δ11B; Foraminifera, planktic δ13C; Foraminifera, planktic δ18O; Joides Resolution; Leg114; Leg143; Leg207; Leg208; Magnesium/Calcium ratio; MECO; Mg/Ca; North Pacific Ocean; Ocean Drilling Program; ODP; planktic foraminifera; Sample code/label; South Atlantic Ocean; Species; Sr/Ca; Strontium/Calcium ratio; Walvis Ridge, Southeast Atlantic Ocean; δ11B, standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 433 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2024-03-15
    Beschreibung: The response of the marine carbon cycle to changes in atmospheric CO2 concentrations will be determined, in part, by the relative response of calcifying and non-calcifying organisms to global change. Planktonic foraminifera are responsible for a quarter or more of global carbonate production, therefore understanding the sensitivity of calcification in these organisms to environmental change is critical. Despite this, there remains little consensus as to whether, or to what extent, chemical and physical factors affect foraminiferal calcification. To address this, we directly test the effect of multiple controls on calcification in culture experiments and core-top measurements of Globigerinoides ruber. We find that two factors, body size and the carbonate system, strongly influence calcification intensity in life, but that exposure to corrosive bottom waters can overprint this signal post mortem. Using a simple model for the addition of calcite through ontogeny, we show that variable body size between and within datasets could complicate studies that examine environmental controls on foraminiferal shell weight. In addition, we suggest that size could ultimately play a role in determining whether calcification will increase or decrease with acidification. Our models highlight that knowledge of the specific morphological and physiological mechanisms driving ontogenetic change in calcification in different species will be critical in predicting the response of foraminiferal calcification to future change in atmospheric pCO2.
    Schlagwort(e): Aragonite saturation state; Area; Benthos; Bicarbonate ion; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcification intensity; Calcification intensity, standard error; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chamber number; Chromista; Coast and continental shelf; Experiment; Foraminifera; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Globigerinoides ruber; Growth/Morphology; Heterotrophic prokaryotes; Laboratory experiment; Magnesium/Calcium ratio; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard error; Red Sea; Salinity; Single species; Species; Temperate; Temperature, water; Type
    Materialart: Dataset
    Format: text/tab-separated-values, 264 data points
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
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