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  • 1
    Type of Medium: Electronic Resource
    Pages: 1 CD-ROM , Booklet (XVII, 30, 49 S.) , 12 cm
    Edition: [Elektronische Ressource]
    Series Statement: Proceedings of the Ocean Drilling Program 182.1998
    Language: English
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  • 2
    Book
    Book
    Tulsa, Okla. : SEPM
    Type of Medium: Book
    Pages: Getr. Zählung
    Series Statement: SEPM short course 12
    Language: English
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  • 3
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    Unknown
    University of South Florida, Department of Marine Science | Gainsville, FL
    In:  http://aquaticcommons.org/id/eprint/30 | 3 | 2020-08-24 02:35:04 | 30 | Florida Sea Grant College Program
    Publication Date: 2021-06-25
    Description: During late August and early September, 1985, Hurricane Elena passed erratically through the Gulf of Mexico, threatening landfall across the west-central Florida coast. This class 3 (maximum winds were 110 knots)hurricane's unusual path caused i t t o remain approximately stationaryabout 100 km off the west-central coast of Florida for 36 hours. Eventually, Elena passed off to the west-northwest making 1 and fall along the Mississippi coast. Hurricane Elena caused the largest evacuation in. U.S. history of people from coastal lowlands. This storm also causedwidespread property damage and is one of the most expensive storms on record. (38pp.)
    Keywords: Atmospheric Sciences ; Oceanography ; Environment ; hurricanes ; Florida ; marsh ; coastal erosion ; mangroves ; Hurricane Elena ; Hurricane Kate
    Repository Name: AquaDocs
    Type: monograph
    Format: application/pdf
    Format: application/pdf
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 26 (1979), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Weekly topographic profile measurements across a southward migrating recurved-spit complex throughout a summer period have revealed three different mechanisms of berm development, each reflected by a distinctive sedimentary sequence. Each mechanism dominates berm widening along certain sections of the active spit with transition zones separating each one. Along the straight beach sections where a net longshore transport is well developed, sand accumulates at the distal high-tide swash mark during neap tide. These sandy accumulations are neap berms which are later redistributed over the main berm by swash occurring at spring high water. The main berm grows vertically and horizontally as a result. To the south, along the middle portion of the recurved spit, swash bars or ridge-and-runnel systems actively develop, migrate, and weld onto the established berms. This is the second method of berm widening and results from an excess of sand carried into this portion of the spit due to the steadily decreasing transport of the longshore current system. Berm-ridges develop along the southernmost portion of the active recurved spit and represent the third and most rapid form of beach progradation. Wide, broad swash bars build nearly up to the spring high tide level. At neap high tide, the swash cannot extend over this feature. Wave energy is expended on the seaward margin of the swash bar initially developing a low-angle beach face. Rapidly, this beach face steepens and a new berm (beach face and berm top) is developed on top of the swash bar. This berm structure still retains much of its swash bar or ridge appearance, hence the term‘berm-ridge'. Numerous trenches dug into the beach provide data to model the distribution of primary sedimentary structures in recurved spits. Berm-ridges are the most important features along rapidly accreting spits, and structures associated with these features are volumetrically the most significant. Berm-ridges also develop arcuate, vegetated ridges separated by low lying, marsh-infilled swales. These features are commonly seen within barrier islands and designate former inlets.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 35 (1988), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Analyses of high resolution, seismic reflection profiles and surface sediment samples indicate that the Cat Island shelf is presently in an incipiently drowned state. This small carbonate bank is characterized by a thin (〈4 m), coarse-grained, relict sediment cover, along with limited reef development, and a relatively deep (20–30 m) margin indicating that it has been unable to ‘keep-up’ with Holocene sea-level rise.Early flooding at relatively high rates of sea-level rise (4 m kyr-1, 5–8 × 103 yr BP) in conjunction with small bank size and relatively low elevation, led to a reduced rate of carbonate accumulation and incipient drowning. The shelf edge currently lies beneath the zone of maximum carbonate production and exposes the interior shelf to open marine conditions which may result in permanent drowning if it is unable to ‘catch-up’ with continued sea-level rise. Sediment facies patterns are largely oriented perpendicular or oblique to the shelf edge and appear to be controlled by shelf circulation patterns focused by bank-margin reentrants.In comparison with most of the northern Bahamas, the Cat Island shelf was flooded earlier and at relatively higher rates of Holocene sea-level rise which led to selective drowning, implying that carbonate platforms need not drown synchronously over widespread areas as commonly thought. The potential rock record of this incipient drowning event would be a thin, open-marine sand sheet of highly degraded cryptocrystalline and aggregate grains associated with poorly developed reefs.
    Type of Medium: Electronic Resource
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: James, Noel P; Feary, David A; Surlyk, Finn; Toni Simo, J A; Betzler, Christian; Holbourn, Ann E; Li, Qianyu; Matsuda, Hiroki; Machiyama, Hideaki; Brooks, Gregg R; Andres, Miriam S; Hine, Albert C; Malone, Mitchell J; Shipboard Scientific Party (2000): Quaternary bryozoan reef mounds in cool-water, upper slope environments: Great Australian Bight. Geology, 28(7), 647-650, https://doi.org/10.1130/0091-7613(2000)28%3C647:QBRMIC%3E2.0.CO;2
    Publication Date: 2023-06-27
    Description: Bryozoan reef mounds are common features in the geological record, occurring within mid-ramp, slope paleoenvironments, especially in Paleozoic carbonate successions, but until now have not been recorded from the modern ocean. Recent scientific drilling in the Great Australian Bight (Ocean Drilling Program Leg 182) has confirmed the existence of shallow subsurface bryozoan reef mounds in modern water depths of 200-350 m. These structures have as much as 65 m of synoptic relief, and occur both as single mounds and as mound complexes. They are unlithified, have a floatstone texture, and are rich in delicate branching, encrusting and/or nodular-arborescent, flat-robust branching, fenestrate, and articulated zooidal bryozoan growth forms. The muddy matrix is composed of foraminifers, serpulids, fecal pellets, irregular bioclasts, sponge spicules, and calcareous nannofossils. The 14C accelerator mass spectrometry dates of 26.6-35.1 ka indicate that the most recent mounds, the tops of which are 7-10 m below the modern seafloor, flourished during the last glacial lowstand but perished during transgressive sea-level rise. This history reflects changing oceanographic current patterns; strong upwelling during lowstands, and reduced upwelling and lowered trophic resources during highstands. Large specimens of benthic foraminifers restricted to the mounds confirm overall mesotrophic growth conditions. The mounds are similar in geometry, scale, general composition, and paleoenvironments to older structures, but lack obvious microbial influence and extensive synsedimentary cementation. Such differences reflect either short-term local conditions or long-term temporal changes in ocean chemistry and biology.
    Keywords: 182-1131B; AGE; Age, standard deviation; Calculated; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Great Australian Bight; Joides Resolution; Leg182; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 7
    Publication Date: 2024-01-09
    Keywords: 182-1134A; AGE; Age, maximum/old; Age, minimum/young; Ageprofile Datum Description; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Great Australian Bight; Joides Resolution; Leg182; Ocean Drilling Program; ODP
    Type: Dataset
    Format: text/tab-separated-values, 370 data points
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  • 8
    Publication Date: 2024-01-09
    Keywords: 182-1126D; Calcium carbonate; Carbon, inorganic, total; Carbon, organic, total; Carbon, total; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Great Australian Bight; Hydrogen; Joides Resolution; Leg182; Nitrogen, total; Ocean Drilling Program; ODP; Sample code/label; Sulfur, total
    Type: Dataset
    Format: text/tab-separated-values, 189 data points
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  • 9
    Publication Date: 2024-01-09
    Keywords: 182-1130C; Calcium carbonate; Carbon, inorganic, total; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Great Australian Bight; Joides Resolution; Leg182; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
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  • 10
    Publication Date: 2024-01-09
    Keywords: 182-1129D; Calcium carbonate; Carbon, inorganic, total; Carbon, organic, total; Carbon, total; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Great Australian Bight; Hydrogen; Joides Resolution; Leg182; Nitrogen, total; Ocean Drilling Program; ODP; Sample code/label; Sulfur, total
    Type: Dataset
    Format: text/tab-separated-values, 171 data points
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