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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing :
    Keywords: Sedimentology. ; Geology. ; Paleontology . ; Earth sciences. ; Oceanography. ; Sedimentology. ; Geology. ; Paleontology. ; Earth Sciences. ; Ocean Sciences.
    Description / Table of Contents: 1. Setting -- 2. Modern Sedimentology -- 3. Cenozoic Depositional Basins -- 4. Geohistory and Sedimentary Successions -- 5. SA2 Eocene – Early Oligocene -- 6. SA3 Upper Ologocene-Mid Miocene -- 7. SA4 Plio-Pleistocene -- 8. Pre-Uplift -- 9. Post Uplift.
    Abstract: This book documents and interprets the onshore Cenozoic temperate carbonate depositional system along the southern margin of Australia. These strata, deposited in four separate basins, together with the extensive modern marine system offshore, comprise the largest such cool-water carbonate system on the globe. The approach is classic and comparative but the information is a synthesis of recent research and new information. A brief section of introduction outlines the setting, modern comparative sedimentology offshore, and structure of the Cenozoic onshore. The core of the book is a detailed analysis and illustration of the four Eocene to Pleistocene successions. Deposits range from temperate carbonates, to biosiliceous spiculites, to marginal marine siliciclastics. Each unit is interpreted, as much as possible, based on our understanding of the modern offshore depositional system. A subsequent part concentrates on diagenesis both before and after the late Miocene uplift. It turns out that alteration in the two packages is entirely different. The preceding attributes of each succession are then interpreted on the basis of controlling factors such as tectonics, oceanography, climate, and glaciation of nearby Antarctica. This research has revealed new implications for the interpretation of specific attributes of cool-water carbonate sedimentology that could only be discovered from the rock record. Insights concerning cyclicity, reef mounds, biosiliceous deposition, and trophic resources are detailed in the next section. The concluding part focuses on global comparisons, especially the Mediterranean and New Zealand.
    Type of Medium: Online Resource
    Pages: XXXII, 217 p. 111 illus., 107 illus. in color. , online resource.
    Edition: 1st ed. 2021.
    ISBN: 9783030639822
    DDC: 551.3
    Language: English
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  • 2
    Call number: SR 90.1028(6)
    In: Smithsonian contributions to the earth sciences
    Type of Medium: Series available for loan
    Pages: 24 S.
    Series Statement: Smithsonian contributions to the earth sciences 6
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Washington, DC : American Geophysical Union
    Associated volumes
    Call number: 9/M 92.1389
    In: Short course in geology
    Type of Medium: Monograph available for loan
    Pages: vii, 160 Seiten , Diagramme
    ISBN: 0875907008
    Series Statement: Short course in geology 4
    Classification:
    Petrology, Petrography
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 4
    Call number: SR 90.0007(366)
    In: Bulletin
    Type of Medium: Series available for loan
    Pages: 143 S. + 4 pl.
    ISBN: 0660121026
    Series Statement: Bulletin / Geological Survey of Canada 366
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 5
    Monograph available for loan
    Monograph available for loan
    St. John's, Newfoundland : Geological Association of Canada
    Call number: M 96.0130
    Type of Medium: Monograph available for loan
    Pages: 454 S.
    Edition: 2nd print.
    ISBN: 0919216498
    Classification:
    Sedimentology
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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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
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    Unknown
    PANGAEA
    In:  Supplement to: Holbourn, Ann E; Kuhnt, Wolfgang; James, Noel P (2002): Late Pleistocene bryozoan reef mounds of the Great Australian Bight: isotope stratigraphy and benthic foraminiferal record. Paleoceanography, 17(3), 1042, https://doi.org/10.1029/2001PA000643
    Publication Date: 2024-01-09
    Description: Cores from Sites 1129, 1131, and 1132 (Ocean Drilling Program (ODP) Leg 182) on the uppermost slope at the edge of the continental shelf in the Great Australian Bight reveal the existence of upper Pleistocene bryozoan reef mounds, previously only detected on seismic lines. Benthic foraminiferal oxygen isotope data for the last 450,000 years indicate that bryozoan reef mounds predominantly accumulated during periods of lower sea level and colder climate since stage 8 at Sites 1129 and 1132 and since stage 4 at the deeper Site 1131. During glacials and interstadials (stages 2-8) the combination of lowered sea level, increased upwelling, and absence of the Leeuwin Current probably led to an enhanced carbon flux at the seafloor that favored prolific bryozoan growth and mound formation at Site 1132. At Site 1129, higher temperatures and downwelling appear to have inhibited the full development of bryozoan mounds during stages 2-4. During that time, favorable hydrographic conditions for the growth of bryozoan mounds shifted downslope from Site 1129 to Site 1131. Superimposed on these glacial-interglacial fluctuations is a distinct long-term paleoceanographic change. Prior to stage 8, benthic foraminiferal assemblages indicate low carbon flux to the seafloor, and bryozoan mounds, although present closer inshore, did not accumulate significantly at Sites 1129 and 1132, even during glacials. Our results show that the interplay of sea level change (eustatic and local, linked to platform progradation), glacial-interglacial carbon flux fluctuations (linked to local hydrographic variations), and possibly long-term climatic change strongly influenced the evolution of the Great Australian Bight carbonate margin during the late Pleistocene.
    Keywords: 182-1129C; 182-1131B; 182-1132B; DRILL; Drilling/drill rig; Great Australian Bight; Joides Resolution; Leg182; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 18 datasets
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  • 8
    Publication Date: 2024-01-09
    Keywords: 182-1127B; 182-1130A; 182-1131A; 182-1131B; 182-1132B; 182-1134A; Age, 14C AMS; Age, dated material; Age, maximum/old; Age, minimum/young; Calculated; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Elevation of event; Event label; Great Australian Bight; Joides Resolution; Latitude of event; Leg182; Longitude of event; Ocean Drilling Program; ODP; Sample comment; Sedimentation rate
    Type: Dataset
    Format: text/tab-separated-values, 215 data points
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  • 9
    Publication Date: 2024-01-09
    Keywords: 182-1130A; Aragonite; DEPTH, sediment/rock; Dolomite; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Great Australian Bight; Joides Resolution; Leg182; Magnesium-Calcite; Ocean Drilling Program; ODP; Sample code/label; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 100 data points
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  • 10
    Publication Date: 2024-01-09
    Keywords: 182-1129C; 182-1131A; 182-1132B; Adeonellopsis spp., δ13C; Adeonellopsis spp., δ18O; corrected to pure calcite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Great Australian Bight; Joides Resolution; Latitude of event; Leg182; Longitude of event; Mass spectrometer Finnigan Delta-S; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 720 data points
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