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  • 1
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    PANGAEA
    In:  Supplement to: Ito, Makoto; O'Connell, Suzanne B; Stefani, Ann; Borella, Peter E (1992): Fluviodeltaic successions at the Wombat Plateau: Upper Triassic siliciclastic-carbonate cycles. In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 109-128, https://doi.org/10.2973/odp.proc.sr.122.139.1992
    Publication Date: 2024-01-09
    Description: The Carnian to Norian sediments, as much as 600 m in total thickness, recovered from ODP Sites 759 and 760 on the Wombat Plateau, are generally represented by fluvial-dominated deltaic successions. In general, the Carnian to Norian sandstones are quartzose. The average ratio of monocrystalline quartz grains, total feldspar grains, and total lithic fragments (i.e., Qm:F:Lt ratio) is 71:22:7. This indicates that they were derived mainly from the transitional continental and cratonic interior provenance terranes, such as the Pilbara Precambrian block to the south of the Wombat Plateau. The upper Carnian sediments, however, are characterized by more feldspathic sandstone petrofacies. They typically contain some volcanic rock fragments with trachytic texture and indicate the onset of the incipient rift-related tectonic movement, such as uplift and subsequent abrupt basin subsidence, together with volcanism in the Gondwana continental block. Mixed siliciclastic and carbonate cycles are typically intercalated in the prodelta to delta front deposits that developed mainly in a lagoon-like, restricted marine environment. The restricted marine environment developed during transgressions as the outflow of shallow water was restricted by depositional barriers. Around the barriers and/or delta lobes, carbonate shoals/banks were probably developed and the allochemical components of the neritic limestones may have been transported into the restricted marine environment by overwash processes and/or storm waves. Siliciclastic detritus, on the other hand, was mainly derived accompanied by delta progradation dominated by fluvial processes in the restricted marine environment. Therefore, we interpret the mixed siliciclastic and carbonate cycles in the deltaic successions to be a result of transgression-regression cycles in a deltaic system during the Late Triassic.
    Keywords: 122-759B; 122-760A; 122-760B; Counting 〉62.5 µm fraction; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Feldspar; Joides Resolution; Kalifeldspar; Leg122; Lithic grains; Metamorphic fragments; Ocean Drilling Program; ODP; Plagioclase; Quartz; Quartz, monocrystalline; Quartz, polycrystalline; Sample code/label; South Indian Ridge, South Indian Ocean; Stage; Volcanic components
    Type: Dataset
    Format: text/tab-separated-values, 696 data points
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  • 2
    Publication Date: 2024-01-09
    Keywords: 122-763C; Counting 〉63 µm fraction; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Feldspar; Glauconite; Joides Resolution; Kalifeldspar; Leg122; Lithic grains; Ocean Drilling Program; ODP; Plagioclase; Quartz; Quartz, monocrystalline; Quartz, polycrystalline; Sample code/label; South Indian Ridge, South Indian Ocean; Volcanic components
    Type: Dataset
    Format: text/tab-separated-values, 451 data points
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  • 3
    facet.materialart.
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    PANGAEA
    In:  Supplement to: Exon, Neville F; Borella, Peter E; Ito, Makoto (1992): Sedimentology of marine Cretaceous sequences in the central Exmouth Plateau (Northwest Australia). In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 233-257, https://doi.org/10.2973/odp.proc.sr.122.144.1992
    Publication Date: 2024-01-09
    Description: Sites 762 and 763 were both drilled on the central Exmouth Plateau in water depths of about 1380 m. At Site 763, 1036 m were drilled about 100 km northeast of the Cuvier Abyssal Plain, and at Site 762, 940 m were drilled about 80 km to the north of Site 763. At both sites we recovered continuous core from fairly complete Cenozoic and Cretaceous sequences; the Cretaceous sequence is 790 m thick in Site 763 and 385 m thick in Site 762. Site 763 has an expanded Early Cretaceous sequence, and Site 762 has an expanded Late Cretaceous sequence. The Cretaceous sequence rests either on a very condensed Jurassic shelf sequence or on Triassic sediments. It commences with Berriasian deltaic mudstone and sandstone (Barrow Group) which built rapidly northward. After late Valanginian breakup of Gondwanaland, there was a hiatus before Hauterivian to early Aptian marine mudstone (Muderong Shale) was deposited following a marine transgression. A late Aptian hiatus was followed by deposition of Albian mudstone and marl (Gearle Siltstone) and late Albian to Coniacian marl (Haycock Marl). Pure pelagic carbonate sedimentation started in the Santonian (Toolonga Calcilutite), and the remainder of the Cretaceous consists of chalks. Sedimentation rates in the Berriasian were about 150 m/m.y. near Site 763 and less to the north. In the remainder of the Cretaceous they seldom exceeded 20 m/m.y. Both tectonic events and eustatic sea-level changes are reflected in the sediments. Color cycles in the marls and chalks can be related to the Milankovitch orbital precession (21 k.y.) and obliquity (41 k.y.) cycles.
    Keywords: 122-762C; 122-763C; DRILL; Drilling/drill rig; Joides Resolution; Leg122; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 4
    Publication Date: 2024-01-09
    Keywords: 122-762C; Carbonate bomb (Müller & Gastner, 1971); Carbonates; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Grain size, SEDIGRAPH 5100; Grain size, sieving; Joides Resolution; Leg122; Median, grain size; Mode, grain size; Ocean Drilling Program; ODP; Sample code/label; Size fraction 〈 0.063 mm, mud, silt+clay; Size fraction 〉 0.063 mm, sand; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: text/tab-separated-values, 346 data points
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  • 5
    Publication Date: 2024-01-09
    Keywords: 122-763C; Carbonate bomb (Müller & Gastner, 1971); Carbonates; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Grain size, SEDIGRAPH 5100; Grain size, sieving; Joides Resolution; Leg122; Median, grain size; Mode, grain size; Ocean Drilling Program; ODP; Sample code/label; Size fraction 〈 0.063 mm, mud, silt+clay; Size fraction 〉 0.063 mm, sand; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: text/tab-separated-values, 336 data points
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 41 (1994), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Palaeo-Tokyo Bay is a relic of the Plio-Pleistocene Kazusa forearc basin in the Boso Peninsula of Japan. The sedimentary infill of palaeo-Tokyo Bay is characterized by shallow marine to paralic sediments of the middle to upper Pleistocene Shimosa Group. Sequence stratigraphical analysis has been used to describe spatial and temporal variations in the depositional systems of the lowest units of the Shimosa Group, deposited during the early stage of development of palaeo-Tokyo Bay.Three different type of depositional systems were recognized: sand ridge to shelf (SRS), shelf to delta (SDL) and shelf to non-deltaic nearshore (SNS) systems. They overlie early transgressive estuarine deposits infilling lowstand valleys incised in the south-eastern margin of palaeo-Tokyo Bay. These systems were developed during late transgressive through highstand stages of a relative sea level cycle, which may have been controlled by a glacio-eustatic sea level change at about 0·4 Ma. Spatial variation in depositional systems is largely identical to that in modern Tokyo Bay; environmental conditions similar to those prevailing at the present day probably characterized the early history of palaeo-Tokyo Bay.The timing of highstand systems tracts within a high frequency depositional sequence was analysed in terms of the effect of sedimentation rate, based on the mapping of a chronostratigraphical surface marked by the Hy4 volcanic ash layer. From spatial variations in sedimentation rate, it was possible to identify the diachronous evolution of highstand systems tracts from the SDL system, through the SNS system, to the SRS system. Time lag is indicated by major bounding surfaces, such as maximum flooding or downlap surfaces associated with a condensed section, which developed immediately above or below the Hy4 volcanic ash layer. The lag may be of the order of a few thousands to tens of thousands of years within a depositional sequence with a total of duration of about 100 000 years.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    FEMS immunology and medical microbiology 34 (2002), S. 0 
    ISSN: 1574-695X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Medicine
    Notes: A longer survival and a decrease in the number of fungal cells in kidneys and brain were observed in groups of mice inoculated with Aspergillus fumigatus conidia 2–3 weeks (especially 3 weeks) after sarcoma 180 tumor transplantation compared to groups of non-tumor-bearing (control) mice inoculated with fungal cells only. The 3–4-week tumor-bearing mice had significantly decreased levels of serum iron and increased levels of unbound iron binding capacity in the serum compared to those of the non-tumor-bearing mice.
    Type of Medium: Electronic Resource
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  • 8
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    Unknown
    Tokyo : Periodicals Archive Online (PAO)
    Japan Quarterly. 6:3 (1959:July/Sept.) 316 
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  • 9
    ISSN: 1573-0832
    Keywords: Cryptococcus neoformans ; ICAM-1 ; intravascular granuloma ; endogenous peroxidase
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine
    Notes: Abstract In rodents an intravenous administration of viableCryptococcus (C.) neoformans cells frequently resulted in attachment of intravascular cryptococcal granulomas to inner walls of the large to medium-sized veins of various organs, including the lungs, liver and spleen. In order to elucidate the pathogenesis of granulomatous changes, the cells composing the intravascular granulomas were observed by electron microscopic peroxidase (PO) cytochemistry. The granuloma composing cells could be divided into the following four types according to the pattern of endogenous peroxidase activity: exudate macrophage (Mφ, type I), PO-negative Mφ (type II), resident Mφ (type III) and other inflammatory cells (type IV). In the intravenous granulomas of the lung, the percentages of composed cells were 39.0% for type I, 57.9% for type II, 0% for type III and 3.1% for type IV. By contrast, in the interstitial granulomas in the lung, type III Mφs, possibly derived from alveolar Mφs, played a significant role in granuloma formation. This may indicate that the intravascular granuloma is almost composed of macrophages derived from monocytes rather than alveolar macrophages. The expression of ICAM-1 on endothelia of the pulmonary veins was examined by immunoelectron microscopy. An immunogold labeling index was significantly augmented on the surface of endothelia in response to intravenous challenge ofC. neoformans. The intravascular granuloma demonstrates that the monocytes develop into the granuloma-composing macrophages and suppress the cryptococcal activities even hi the peripheral blood resulting in an assistance of endothelial functions.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1573-6865
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine
    Notes: Summary Inner ears from neonatal and adult Mongolian gerbils were examined to determine developmental changes in the content of glycogen and glycoconjugates as shown by histochemical application of the jack bean lectin, concanavalin A (con A). Sections of fixed paraffin-embedded inner ears were stained using the con A-horseradish peroxidase sequence in conjunction with prior treatments including periodate oxidation with or without subsequent reduction and diastase digestion. In adult inner ear, brief periodate oxidation followed by reduction and con A-horseradish peroxidase staining demonstrated abundant glycogen in Deiters' cells and in fibrocytes of the spiral ligament and submacular plaque. This procedure also detected diastase-resistant glycoprotein, probably containing N-linked complex-type saccharides, in the basal and marginal regions of the tectorial membrane and in the otolithic membrane. During morphogenesis and maturation, various cochlear cells showed changes in their glycogen content possibly related to stage-specific energy requirements. Cellular glycogen storage reached adult levels by postnatal day 14. The tectorial membrane gradually acquired con A reactivity during the first postnatal week. Thus, application of modified con A staining procedures has provided further knowledge for comparison with data from previous biochemical and histochemical studies of carbohydrate-rich components in the inner ear.
    Type of Medium: Electronic Resource
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