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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 43 (1996), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Coeval stratigraphic units of similar petrology occur throughout the northern Bahamas islands. The petrographic composition of these limestones provides clues about regional sea level and climate changes during the late Quaternary. At least eight fossil shoreline units, which are linked to transgressive episodes between the middle Pleistocene and the late Holocene, are recognized in the Bahamas. The petrographic composition of these units is either dominated by ooids and peloids or by bioclasts. Sedimentological observations demonstrate that oolitic-peloidal units were formed when sea level was higher than today, whereas skeletal units were deposited at or below modern ordnance datum. Skeletal units may reflect times of partial, or modest platform flooding, when the bulk of sediments brought to islands originates from bank-margin reefs. In contrast, oolitic-peloidal units correspond to major flooding events and active water circulation on the bank top. Cement fabrics further show that the early diagenesis of oolitic units took place during warm and humid climatic conditions, whereas skeletal rock bodies underwent subaerial diagenesis during drier climatic conditions characterized by marked seasonal changes. This example from the Bahamas suggests that compositional analysis of limestone from fossil carbonate platforms could be used for resolving ancient climate and sea-level changes.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2024-01-09
    Keywords: 194-1195A; Braarudosphaera bigelowii; Calcidiscus leptoporus; Calciosolenia brasiliensis; Calciosolenia murrayi; Ceratolithus cristatus; Ceratolithus telesmus; Coral Sea; DEPTH, sediment/rock; Discosphaera tubifer; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Emiliania huxleyi; Florisphaera profunda; Gephyrocapsa caribbeanica; Gephyrocapsa oceanica; Gephyrocapsa spp.; Hayaster perplexus; Helicosphaera carteri; Helicosphaera hyalina; Helicosphaera inversa; Helicosphaera neogranulata; Helicosphaera pavimentum; Helicosphaera wallichii; Holodiscolithus macroporus; Joides Resolution; Leg194; Nannofossil abundance; Nannofossils preservation; Neosphaera coccolithomorpha; Ocean Drilling Program; ODP; Oolithotus antillarum; Oolithotus fragilis; Pontosphaera discopora; Pontosphaera japonica; Pontosphaera multipora; Pontosphaera sp.; Pseudoemiliania lacunosa; Reticulofenestra sp.; Rhabdosphaera clavigera; Rhabdosphaera sp.; Sample code/label; Scyphosphaera aequatorialis; Scyphosphaera apsteinii; Scyphosphaera apsteinii dilatata; Scyphosphaera porosa; Siliceous spicules; Smear slide analysis; Syracosphaera histrica; Thoracosphaera spp.; Umbellosphaera irregularis; Umbellosphaera tenuis; Umbilicosphaera hulburtiana; Umbilicosphaera sibogae var. foliosa; Umbilicosphaera sibogae var. sibogae
    Type: Dataset
    Format: text/tab-separated-values, 1920 data points
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  • 3
    Publication Date: 2024-01-09
    Keywords: 194-1195A; Aragonite; Calcite; Coral Sea; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Kaolinite; Leg194; Magnesium-Calcite; Ocean Drilling Program; ODP; Quartz; Sample code/label; Truncorotalia tosaensis; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 180 data points
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Dubois, Nathalie; Kindler, Pascal; Spezzaferri, Silvia; Coric, Stjepan (2008): The initiation of the southern central Great Barrier Reef: New multiproxy data from Pleistocene distal sediments from the Marion Plateau (NE Australia). Marine Geology, 250(3-4), 223-233, https://doi.org/10.1016/j.margeo.2008.01.007
    Publication Date: 2024-01-09
    Description: Significant synchronous shifts in the chemistry, mineralogy, grain sizes and color of the sediments at 6 m below sea floor (mbsf) at ODP Site 1195 on the Marion Plateau (NE Australia) are interpreted to reflect a major regional paleoceanographic change: the initiation of the southern province of the Great Barrier Reef (GBR). The onset of this massive carbonate production centre nearby resulted primarily in increased deposition of carbonate-rich sediments of neritic origin. Both sedimentation rate and terrigenous input record a coincident decline attributed to inshore trapping of materials behind the reefs. Our best estimate places the development of reef framework in the southern part of the GBR between 560 and 670 kyr B.P., based on an age model combining magnetostratigraphic and biostratigraphic data. The proposed estimation agrees with previous studies reporting an age between 500 and 930 kyr B.P., constraining more tightly their results. However, it does not support research placing the birth of the GBR in Marine Isotope Stage (MIS) 11 (~400 kyr), nor the theory of a worldwide modern barrier reef development at that time.
    Keywords: 194-1195A; Coral Sea; DRILL; Drilling/drill rig; Joides Resolution; Leg194; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 5
    Publication Date: 2011-06-01
    Description: We report here the discovery of Miocene, Pliocene, and early Pleistocene shallow-marine carbonates on Mayaguana Island (southeastern Bahamas) that have so far not been observed on any other Bahamian island. Spanning more than 17 m.y., but
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
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