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  • PANGAEA  (11)
  • Amsterdam [u.a.] : Elsevier  (1)
  • 2010-2014  (12)
Document type
Keywords
Publisher
Language
Years
Year
  • 1
    Book
    Book
    Amsterdam [u.a.] : Elsevier
    Type of Medium: Book
    Pages: VI, 194 S , Ill., graph. Darst
    Series Statement: Marine chemistry 120.2010,1/4
    Language: English
    Location Call Number Limitation Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Griffith, Elizabeth M; Calhoun, Michael; Thomas, Ellen; Averyt, Kristen; Erhardt, Andrea M; Bralower, Timothy J; Lyle, Mitchell W; Olivarez Lyle, Annette; Paytan, Adina (2010): Export productivity and carbonate accumulation in the Pacific Basin at the transition from a greenhouse to icehouse climate (late Eocene to early Oligocene). Paleoceanography, 25(3), PA3212, https://doi.org/10.1029/2010PA001932
    Publication Date: 2024-07-19
    Description: The late Eocene through earliest Oligocene (40-32 Ma) spans a major transition from greenhouse to icehouse climate, with net cooling and expansion of Antarctic glaciation shortly after the Eocene/Oligocene (E/O) boundary. We investigated the response of the oceanic biosphere to these changes by reconstructing barite and CaCO3 accumulation rates in sediments from the equatorial and North Pacific Ocean. These data allow us to evaluate temporal and geographical variability in export production and CaCO3 preservation. Barite accumulation rates were on average higher in the warmer late Eocene than in the colder early Oligocene, but cool periods within the Eocene were characterized by peaks in both barite and CaCO3 accumulation in the equatorial region. We infer that climatic changes not only affected deep ocean ventilation and chemistry, but also had profound effects on surface water characteristics influencing export productivity. The ratio of CaCO3 to barite accumulation rates, representing the ratio of particulate inorganic C accumulation to Corg export, increased dramatically at the E/O boundary. This suggests that long-term drawdown of atmospheric CO2 due to organic carbon deposition to the seafloor decreased, potentially offsetting decreasing pCO2 levels and associated cooling. The relatively larger increase in CaCO3 accumulation compared to export production at the E/O suggests that the permanent deepening of the calcite compensation depth (CCD) at that time stems primarily from changes in deep water chemistry and not from increased carbonate production.
    Keywords: Deep Sea Drilling Project; DSDP; Ocean Drilling Program; ODP
    Type: dataset publication series
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  Supplement to: Erhardt, Andrea M; Pälike, Heiko; Paytan, Adina (2013): High-resolution record of export production in the eastern equatorial Pacific across the Eocene-Oligocene transition and relationships to global climatic records. Paleoceanography, 28(1), 130-142, https://doi.org/10.1029/2012PA002347
    Publication Date: 2024-07-19
    Description: Understanding changes in export production through time provides insight into the response of the biological pump to global climate change, particularly during periods of rapid climate change. In this study we consider what role changes in export production may have had on carbon sequestration and how this may have contributed to the onset of the Eocene-Oligocene transition (EOT). In addition, we consider if these export production variations are dominantly controlled by orbitally driven climate variability. To accomplish these objectives, we report changes in export production in the Eastern Equatorial Pacific (EEP) from Site U1333 across the EOT reconstructed from a high-resolution record of marine barite accumulation rates (BAR). BAR fluctuations suggest synchronous declines in export production associated with the two-step increases in oxygen isotopes that define the transition. The reduction in productivity across the EOT suggests that the biological pump did not contribute to carbon sequestration and the cooling over this transition. We also report a previously undocumented peak in EEP export productivity before the EOT onset. This peak is consistent with export production proxies from the Southern Ocean, potentially implying a global driver for this precursor event. We propose that this enhanced export production and the associated carbon sequestration in the late Eocene may have contributed to the pCO2 drawdown at the onset of Antarctic glaciation.
    Keywords: 320-U1333C; Accumulation rate, barite; Accumulation rate, mass; AGE; Age, reference; Barite; Density, dry bulk; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Exp320; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Mass; Pacific Equatorial Age Transect I; Sample code/label; Sample mass; Sedimentation rate
    Type: dataset
    Format: text/tab-separated-values, 3038 data points
    Location Call Number Limitation Availability
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  • 4
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    PANGAEA
    In:  Supplement to: Averyt, Kristen; Calhoun, Michael; Schmalz, Lyndsie; Paytan, Adina (2005): Data report: Carbonate and barite trends across the Eocene/Oligocene boundary at Shatsky Rise, ODP Leg 198. In: Bralower, TJ; Premoli Silva, I; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 198, 1-16, https://doi.org/10.2973/odp.proc.sr.198.106.2005
    Publication Date: 2024-07-22
    Description: The barite and CaCO3 content (in weight percent) of marine sediments can be used to determine spatial and temporal changes in export production (organic and carbonate carbon flux) and/or CaCO3 preservation (inorganic carbon burial). Here we report barite and CaCO3 content in Eocene/Oligocene (E/O) boundary sediments from locations drilled on Shatsky Rise during Ocean Drilling Program Leg 198. Records of these indexes may be used along with other data to determine how the major E/O boundary climatic transition (initiation of Antarctic glaciation and resultant ocean-climate system changes) affected marine export production/preservation at Shatsky Rise. Such data are necessary to elucidate the timing and phasing of changes in the carbon cycle relative to fluctuations in oceanographic conditions across this climatically important interval.
    Keywords: 198-1209A; 198-1209B; 198-1209C; 198-1210A; 198-1210B; 198-1211A; 198-1211B; 198-1211C; DRILL; Drilling/drill rig; Joides Resolution; Leg198; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: dataset publication series
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-07-23
    Keywords: 198-1209A; 198-1209B; 198-1210A; 198-1210B; 198-1211; 199-1218A; 85-574C; Accumulation rate, barite; Accumulation rate, calcium carbonate; Accumulation rate, mass; Aralia sp.; Barite; Calcium carbonate; Calculated; COMPCORE; Composite Core; Coulometry; Deep Sea Drilling Project; Density, dry bulk; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Joides Resolution; Latitude of event; Leg198; Leg199; Leg85; Longitude of event; North Pacific/TROUGH; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Sequential leaching technique
    Type: dataset
    Format: text/tab-separated-values, 1352 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2024-07-19
    Keywords: 198-1209B; 198-1210B; 198-1211B; AGE; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Grain size, sieving; Joides Resolution; Leg198; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Size fraction 〉 0.063 mm, sand
    Type: dataset
    Format: text/tab-separated-values, 180 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2024-07-22
    Keywords: Bottle, Niskin; Calculated after Luo et al. (2012); Date/Time of event; DEPTH, water; Diazotrophs, total biomass as carbon; Event label; Fluorescence-based quantitative real-time PCR (qPCR); Latitude of event; Longitude of event; Malkat-Shva2005-09-06; Malkat-Shva2005-09-07; MAREDAT_Diazotrophs_Collection; NIS; Red Sea/Gulf of Aqaba; Trichodesmium, abundance expressed in number of nifH gene copies; Trichodesmium, biomass as carbon; Trichodesmium abundance, total
    Type: dataset
    Format: text/tab-separated-values, 24 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-07-22
    Keywords: 198-1209; 198-1210; 198-1211; Age model; Ageprofile Datum Description; COMPCORE; Composite Core; DEPTH, sediment/rock; Event label; Joides Resolution; Leg198; North Pacific Ocean; Ocean Drilling Program; ODP; Reference/source
    Type: dataset
    Format: text/tab-separated-values, 39 data points
    Location Call Number Limitation Availability
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  • 9
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    PANGAEA
    In:  Supplement to: Crook, Elizabeth Derse; Cooper, H; Potts, Donald C; Lambert, T; Paytan, Adina (2013): Impacts of food availability and pCO2 on planulation, juvenile survival, and calcification of the azooxanthellate scleractinian coral Balanophyllia elegans. Biogeosciences, 10(11), 7599-7608, https://doi.org/10.5194/bg-10-7599-2013
    Publication Date: 2024-07-22
    Description: Ocean acidification, the assimilation of atmospheric CO2 by the oceans that decreases the pH and CaCO3 saturation state (Omega) of seawater, is projected to have severe adverse consequences for calcifying organisms. While strong evidence suggests calcification by tropical reef-building corals containing algal symbionts (zooxanthellae) will decline over the next century, likely responses of azooxanthellate corals to ocean acidification are less well understood. Because azooxanthellate corals do not obtain photosynthetic energy from symbionts, they provide a system for studying the direct effects of acidification on energy available for calcification. The solitary azooxanthellate orange cup coral Balanophyllia elegans often lives in low-pH, upwelled waters along the California coast. In an 8-month factorial experiment, we measured the effects of three pCO2 treatments (410, 770, and 1220 µatm) and two feeding frequencies (3-day and 21-day intervals) on "planulation" (larval release) by adult B. elegans, and on the survival, skeletal growth, and calcification of newly settled juveniles. Planulation rates were affected by food level but not pCO2. Juvenile mortality was highest under high pCO2 (1220 µatm) and low food (21-day intervals). Feeding rate had a greater impact on calcification of B. elegans than pCO2. While net calcification was positive even at 1220 µatm (~3 times current atmospheric pCO2), overall calcification declined by ~25-45%, and skeletal density declined by ~35-45% as pCO2 increased from 410 to 1220 µatm. Aragonite crystal morphology changed at high pCO2, becoming significantly shorter but not wider at 1220 µatm. We conclude that food abundance is critical for azooxanthellate coral calcification, and that B. elegans may be partially protected from adverse consequences of ocean acidification in habitats with abundant heterotrophic food.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Animalia; Aragonite saturation state; Aragonite saturation state, standard deviation; Balanophyllia elegans; Benthic animals; Benthos; Bicarbonate ion; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cnidaria; Coulometric titration; Density; Density, standard error; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Identification; Individuals; Laboratory experiment; Laboratory strains; Larvae; Length; Length, standard error; Mass; Mass, standard error; Mortality/Survival; Nitrate; Nitrate, standard deviation; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Other; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard deviation; Phosphate; Phosphate, standard deviation; Potentiometric titration; Proportion; Reproduction; Salinity; Salinity, standard deviation; Silicate; Silicate, standard deviation; Single species; Species; Table; Temperature, water; Temperature, water, standard deviation; Treatment; Volume; Volume, standard error; Width; Width, standard error
    Type: dataset
    Format: text/tab-separated-values, 20615 data points
    Location Call Number Limitation Availability
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  • 10
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    PANGAEA
    In:  Supplement to: Crook, Elizabeth Derse; Cohen, Anne L; Rebolledo-Vieyra, Mario; Hernandez, Laura; Paytan, Adina (2013): Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification. Proceedings of the National Academy of Sciences, 110(27), 11044-11049, https://doi.org/10.1073/pnas.1301589110
    Publication Date: 2024-07-22
    Description: As the surface ocean equilibrates with rising atmospheric CO2, the pH of surface seawater is decreasing with potentially negative impacts on coral calcification. A critical question is whether corals will be able to adapt or acclimate to these changes in seawater chemistry. We use high precision CT scanning of skeletal cores of Porites astreoides, an important Caribbean reef-building coral, to show that calcification rates decrease significantly along a natural gradient in pH and aragonite saturation (Omega arag). This decrease is accompanied by an increase in skeletal erosion and predation by boring organisms. The degree of sensitivity to reduced Oarag measured on our field corals is consistent with that exhibited by the same species in laboratory CO2 manipulation experiments. We conclude that the Porites corals at our field site were not able to acclimatize enough to prevent the impacts of local ocean acidification on their skeletal growth and development, despite spending their entire lifespan in low pH, low Omega arag seawater.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Animalia; Aragonite saturation state; Aragonite saturation state, standard deviation; Benthic animals; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate; Calcification rate, ratio; Calcification rate, standard deviation; Calcification rate, standard error; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cnidaria; Density; Density, standard deviation; Density, standard error; Field observation; Figure; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Linear extension; Linear extension, standard deviation; Linear extension, standard error; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Porites astreoides; Salinity; Single species; Species; Temperature, water; Thickness; Thickness, standard deviation; Thickness, standard error; Treatment; Tropical; Volume ratio
    Type: dataset
    Format: text/tab-separated-values, 479 data points
    Location Call Number Limitation Availability
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