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  • 1
    Book
    Book
    Leiden : Nationaal Natuurhistorisch Museum Naturalis
    Keywords: Foraminifera ; Hochschulschrift ; Tropen ; Benthos ; Foraminiferen ; Biogeografie ; Tropen ; Fossile Foraminiferen ; Paläobiogeografie ; Paläoozeanographie ; Palökologie ; Tropen ; Benthos ; Foraminiferen ; Biogeografie ; Tropen ; Fossile Foraminiferen ; Paläobiogeografie ; Paläoozeanographie ; Palökologie
    Type of Medium: Book
    Pages: 263 S , Ill., graph. Darst
    Series Statement: Scripta Geologica 124
    RVK:
    Language: English
    Note: Zugl.: Amsterdam, Univ., Diss., 2002
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  • 2
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Paleobiogeography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (425 pages)
    Edition: 1st ed.
    ISBN: 9781402063749
    Series Statement: Topics in Geobiology Series ; v.29
    DDC: 591.9
    Language: English
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  • 3
    Publication Date: 2011-09-01
    Description: Persistence in the structure of ecological communities can be predicted both by deterministic and by stochastic theory. Evaluating ecological patterns against the neutral theory of biodiversity provides an appropriate methodology for differentiating between these alternatives. We traced the history of benthic foraminiferal communities from the Huon Peninsula, Papua New Guinea. From the well-preserved uplifted reef terrace at Bonah River we reconstructed the benthic foraminiferal communities during a 2200-year period (9000-6800 yr B.P.) of reef building during the Holocene transgressive sea-level rise. We found that the similarity of foraminiferal communities was consistently above 60%, even when comparing communities on either side of a massive volcanic eruption that smothered the existing reef system with ash. Similarly, species diversity and rank dominance were unchanged through time. However, similarity dropped dramatically in the final stages of reef growth, when accommodation space was reduced as sea-level rise slowed. We compared the community inertia index (CII) computed from the observed species abundances with that predicted from neutral theory. Despite the differences in foraminiferal community composition in the younger part of the reef sequence, we found an overall greater degree of community inertia with less variance in observed communities than was predicted from neutral theory, regardless of foraminiferal community size or species migration rate. Thus, persistent species assemblages could not be ascribed to neutral predictions. Ecological incumbency of established foraminiferal species likely prevented stochastic increases in both migrant and rare taxa at the Bonah River site. Regardless of the structuring mechanisms, our reconstruction of Holocene foraminiferal assemblages provides historical context for the management and potential restoration of degraded species assemblages.
    Print ISSN: 0094-8373
    Electronic ISSN: 0094-8373
    Topics: Geosciences
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  • 4
    Publication Date: 2023-08-12
    Keywords: AII-42-15-14; AII-60-10; Area; Catalog Number; CH82-21; Code; Event label; EW9303-04; IPE.08178; IPE.08199; IPE.08212; IPE.08231; IPE.08316; IPE.08379; KC78; Latitude of event; Length, major axis; Length, minor axis; Longitude of event; North Atlantic; Perimeter; Sample code/label; Size fraction; South Atlantic; Species; VM20-248
    Type: Dataset
    Format: text/tab-separated-values, 15544 data points
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  • 5
    Publication Date: 2023-08-12
    Keywords: AII-42-15-14; AII-60-10; Catalog Number; CH82-21; Code; Event label; EW9303-04; Height; IPE.08178; IPE.08199; IPE.08212; IPE.08231; IPE.08316; IPE.08379; KC78; Latitude of event; Length; Longitude of event; North Atlantic; Sample code/label; Size fraction; South Atlantic; Species; Surface area, cone; Surface area, cylinder; Surface area, dome; Surface area, ellipse; Surface area, top; VM20-248; Volume, cone; Volume, cylinder; Volume, dome; Volume, ellipse; Volume, top; Width
    Type: Dataset
    Format: text/tab-separated-values, 18150 data points
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  • 6
    Publication Date: 2023-08-12
    Keywords: Area; Axis 1; Axis 2; Axis 3; Sample code/label; Surface area; Surface area per volume; Volume
    Type: Dataset
    Format: text/tab-separated-values, 144 data points
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  • 7
    Publication Date: 2023-08-12
    Keywords: AII-42-15-14; AII-60-10; Catalog Number; CH82-21; Code; Crop area; Event label; EW9303-04; IPE.08178; IPE.08199; IPE.08212; IPE.08231; IPE.08316; IPE.08379; KC78; Latitude of event; Longitude of event; North Atlantic; Number of pores; Pore area; Pore density; Pore size, maximum; Pore size, mean; Pore size, minimum; Pore size, standard deviation; Porosity, foraminiferal; Sample code/label; Scale; Size fraction; South Atlantic; Species; VM20-248
    Type: Dataset
    Format: text/tab-separated-values, 9755 data points
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  • 8
    Publication Date: 2023-08-12
    Keywords: Chamber number; Pore density; Pore size, mean; Porosity, foraminiferal; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 315 data points
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  • 9
    Publication Date: 2023-08-12
    Description: The clustering of mitochondria near pores in the test walls of foraminifera suggests that these perforations play a critical role in metabolic gas exchange. As such, pore measurements could provide a novel means of tracking changes in metabolic rate in the fossil record. However, in planktonic foraminifera, variation in pore size, density, and porosity have been variously attributed to environmental, biological, and taxonomic drivers, complicating such an interpretation. Here we examine the environmental, biological, and evolutionary determinants of porosity in 718 individuals representing 17 morphospecies of planktonic foraminifera from 6 core tops in the North Atlantic. Using random forest models, we find that porosity is primarily correlated to size and habitat temperature, two key factors in determining metabolic rates. In order to test if this correlation arose spuriously through the association of cryptic species with distinct biomes, we cultured Globigerinoides ruber in three different temperature conditions, and found that porosity increased with temperature. Crucially, these results show that porosity can be plastic: changing in response to environmental drivers within the lifetime of an individual foraminifer. This demonstrates the potential of porosity as a proxy for foraminiferal metabolic rates, with significance for interpreting geochemical data and the physiology of foraminifera in non-analog environments. It also highlights the importance of phenotypic plasticity (i.e., ecophenotypy) in accounting for some aspects of morphological variation in the modern and fossil record.
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 10
    Publication Date: 2024-03-19
    Description: Shelled pteropods are widely regarded as bioindicators for ocean acidification, because their fragile aragonite shells are susceptible to increasing ocean acidity. While short-term incubations have demonstrated that pteropod calcification is negatively impacted by ocean acidification, we know little about net calcification in response to varying ocean conditions in natural populations. Here, we examine in situ calcification of Limacina helicina pteropods collected from the California Current Ecosystem, a coastal upwelling system with strong spatial gradients in ocean carbonate chemistry, dissolved oxygen and temperature. Depth-averaged pH ranged from 8.03 in warmer offshore waters to 7.77 in cold CO2-rich waters nearshore. Based on high-resolution micro-CT technology, we showed that shell thickness declined by 37% along the upwelling gradient from offshore to nearshore water. Dissolution marks covered only 2% of the shell surface area and were not associated with the observed variation in shell thickness. We thus infer that pteropods make thinner shells where upwelling brings more acidified and colder waters to the surface. Probably the thinner shells do not result from enhanced dissolution, but are due to a decline in calcification. Reduced calcification of pteropods is likely to have major ecological and biogeochemical implications for the cycling of calcium carbonate in the oceans.
    Keywords: Alkalinity, total; Animalia; Aragonite saturation state; Bicarbonate ion; Calcification/Dissolution; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Diameter; Dissolution; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Height; Identification; LATITUDE; Limacina helicina; Location; LONGITUDE; Mollusca; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Phosphate; Registration number of species; Salinity; Shell, number of whorls; Shell surface area; Shell thickness; Silicate; Single species; Species; Station label; Temperate; Temperature, water; Type; Uniform resource locator/link to reference; Upwelling; Zooplankton
    Type: Dataset
    Format: text/tab-separated-values, 2250 data points
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