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  • 1
    In: Earth & planetary science letters, Amsterdam [u.a.] : Elsevier, 1966, 259(2007), 3/4, Seite 432-441, 0012-821X
    In: volume:259
    In: year:2007
    In: number:3/4
    In: pages:432-441
    Type of Medium: Article
    Pages: Graph. Darst.
    ISSN: 0012-821X
    Language: English
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Gerodontology 9 (1990), S. 0 
    ISSN: 1741-2358
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Normal gingival tissues of BNL mice of different ages were studied, using recently developed immunohistochemical techniques to detect T and B lymphocytes, Langerhans cells and macrophages. The presence of mast cells, plasma cells and neutrophils was also determined. Cell densities were determined in the epithelium and connective tissue compartments of the attachment area, the papilla and the diastema. T lymphocytes (Lyt 1*) were present in the epithelium and connective tissue of all three areas studied. Their numbers increased significantly with age in the attachment area and in the papillary connective tissue. Langerhans cells (F4/80*) were detected in the epithelium of all three areas examined. Their numbers did not vary significantly with age. The highest concentrations of T lymphocytes and Langerhans cells were observed in the attachment area at all ages. Macrophages (F4/80*) were detected in the connective tissue of all three areas examined. Their numbers increased significantly in the papillary connective tissue of older animals (78 weeks of age). Neither B lymphocytes (RA-2C2′) nor plasma cells were detected in any of the tissue areas examined. The presence of neutrophils in the attachment area increased with age. Mast cells were present in all samples in the more vascularized areas (the papilla and diastema). The results suggest that, throughout the lifespan, T lymphocytes, macrophages, Langerhans cells and mast cells are normal constituents of the oral mucosa of the mouse, while B lymphocytes, plasma cells and, for the most part, neutrophils are absent under normal conditions. Furthermore, the concentrations of T lymphocytes and macrophages increased with age in the areas adjacent to the dentition, possibly as a result of reduced tissue resistance to external antigens.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    New York, NY [u.a.] : Wiley-Blackwell
    The @Anatomical Record 197 (1980), S. 283-288 
    ISSN: 0003-276X
    Keywords: Life and Medical Sciences ; Cell & Developmental Biology
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Medicine
    Notes: Histosol is a non-flammable solvent mixture of synthetic aromatic hydrocarbons with a flash point of 124°F (T.C.C.). It has a lower vapor pressure and evaporation rate than other organic solvents, such as xylene, routinely used as clearing and deparaffinizing agents. Although both xylene and Histosol clear and deparaffinize soft organ tissues effectively in the preparation of permanently mounted stained slides, Histosol appears, in many instances, to be the choice solvent: tissues are easier to section; cell bordrs and cell surface modifications are most distinct; cytoplasmic eosinophilia is more vivid; and nuclear detail is improved. Of prime importance, Histosol is a safer and more efficient solvent for use in histological and pathological laboratories.
    Additional Material: 4 Ill.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 0002-9106
    Keywords: Life and Medical Sciences ; Cell & Developmental Biology
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Medicine
    Notes: Erythropoietin (Ep) is produced mainly by the liver and spleen during fetal and neonatal periods and by the kidney during adolescent and adult life. The liver is also an important extrarenal producer of Ep in the hypoxic, anephric adult animal. Subtotal hepatectomy results in a substantial elevation in serum Ep levels at 30-72 hours after hepatectomy in rats subsequently nephrectomized and rendered hypoxic. Ep production is related to the mass of regenerating liver with peak Ep production occurring during times of greatest tissue proliferation. Regenerative and erythropoietic responses to hepatectomy decline with advancing age. Rats undergoing repeated hepatectomies do not recover full liver mass but the initial rate of regeneration increases following each successive hepatectomy. Ep levels decline in anephric hypoxic rats undergoing multiple hepatectomies when compared to sham-operated controls.
    Additional Material: 2 Ill.
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2024-05-06
    Keywords: 188-1165B; 188-1165C; Accumulation rate, ice rafted debris; AGE; Density, dry bulk; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Indian Ocean; Joides Resolution; Leg188; Ocean Drilling Program; ODP; Sample code/label; Sample code/label 2; Sedimentation rate; Size fraction 〉 0.150 mm
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
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  • 6
    Publication Date: 2024-05-06
    Keywords: 188-1165B; 188-1165C; AGE; Age, 40Ar/39Ar Argon-Argon; Age, dated; Age, dated standard deviation; Argon-40; Calcium/Magnesium ratio; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Indian Ocean; Joides Resolution; Leg188; Ocean Drilling Program; ODP; Run; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 2190 data points
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  • 7
    Publication Date: 2024-05-06
    Keywords: 28-268; Age, 40Ar/39Ar Argon-Argon; Age, dated; Age, dated standard deviation; Antarctic Ocean/CONT RISE; Argon-40; Calcium/Magnesium ratio; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg28; Run; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 192 data points
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  • 8
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    In:  Supplement to: Williams, Trevor J; van de Flierdt, Tina; Hemming, Sidney R; Chung, Elena; Roy, Martin; Goldstein, Steven L (2010): Evidence for iceberg armadas from East Antarctica in the Southern Ocean during the late Miocene and early Pliocene. Earth and Planetary Science Letters, 290(3-4), 351-361, https://doi.org/10.1016/j.epsl.2009.12.031
    Publication Date: 2024-05-06
    Description: Sediments from Ocean Drilling Program Site 1165 in the Indian Ocean sector of the Southern Ocean (off Prydz Bay) contain a series of layers that are rich in ice-rafted debris (IRD). Here we present evidence that IRD-rich layers at Site 1165 at 7, 4.8, and 3.5 Ma record short-lived, massive discharges of icebergs from Wilkes Land and Adélie Land, more than 1500 kilometers to the east of the depositional site. This distant source of icebergs is clearly defined by the presence of IRD hornblende grains with 40Ar/39Ar ages of 1200-1100 Ma and 1550-1500 Ma, ages that are not found on the East Antarctic continent in locations closer to Site 1165. This observation requires enormous amounts of detritus-carrying drifting icebergs, most likely in the form of large icebergs. These events probably reflect destabilization, surge, and break-up of ice streams on the Wilkes Land and Adélie Land margins of the East Antarctic Ice Sheet, in the vicinity of the low-lying Aurora and Wilkes Basins. They occurred under warming conditions, but each coast seems to have produced ice-rafting events independently, at different times. The data presented here constitute the first evidence of far-traveled icebergs from specific source areas around the East Antarctic perimeter. Launch of these icebergs may have happened during quite dramatic events, perhaps analogous to "Heinrich Events" in the North Atlantic.
    Keywords: Deep Sea Drilling Project; DSDP; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 9
    Publication Date: 2024-04-20
    Description: The postglacial rebound is component of the glacial isostatic adjustment which causes the Earth's crust to rebound in regions formerly covered by or adjacent to ice sheets, and subside beneath ocean basins. In North America, the observed postglacial rebound is mainly the result of the Laurentide Ice Sheet deglaciation after it reached its maximum thickness and extent at the Last Glacial Maximum (26.5-19 ka). Global-scale numerical models of glacial isostatic adjustment faithfully reproduce past and current changes in postglacial rebound, but the integration their predictions in a geographic information system to facilitate high-resolution paleotopographic reconstructions remains challenging. We therefore present high-resolution raster datasets of land-deformation and ice-free paleotopography of glaciated North America for several time slices since the Last Glacial Maximum to support geological, paleoenvironmental and archeological studies.
    Keywords: Binary Object; Binary Object (File Size); File content; ICE-xG_N-America_LGM; Model
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
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  • 10
    Publication Date: 2017-01-30
    Description: Global Nd–Hf isotope systematics can be mainly described with two linear arrays, the global silicate Earth array (“the terrestrial array”) and the global ferromanganese crust and nodule array (”the seawater array”). The offset between these two arrays provides evidence for the sources and mechanisms by which these elements are added to ocean water. However, the reason for this offset is under debate, with the two preferred hypotheses being (i) incongruent release of Hf during continental weathering and (ii) hydrothermal contribution of Hf to the seawater budget. Here we present new Nd and Hf isotope data on glacio-marine core-top sediments from around the perimeter of the Antarctic continent. The results range from εHf = − 30.0 to εHf = + 3.9 and εNd = − 21.3 to εNd = + 0.9, reflecting the large range of basement ages and lithologies around the Antarctic continent. In Nd–Hf isotope space, they confirm the systematic correlations found in rocks from other parts around the world and provide valuable insights into the previously underrepresented group of sediments with very old provenance. In this paper we revisit the cause for the offset of the seawater array from the terrestrial array using simple mass balance considerations. We use these calculations to test to what degree the seawater array could be a product of preferential weathering of “non-zircon portions” of the upper continental crust, implying retention of zircons in the solid residue of weathering. Lutetium–Hf and Sm–Nd evolution and mixing calculations show that the global seawater array can be generated with continental sources only. On the other hand, a predominantly hydrothermal origin of Hf in the ocean is not possible because the seawater Hf isotopic composition is significantly less radiogenic than hydrothermal sources, and requires a minimum fraction of 50% continental Hf. While hydrothermal sources may contribute some Hf to seawater, continental contributions are required to balance the budget.
    Type: Article , PeerReviewed
    Format: text
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