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  • 1
    Series available for loan
    Series available for loan
    Data update in a land information network (1988)
    Kensington
    Associated volumes
    Details Availability
    Call number: SR 90.0093(S34)
    In: UNISURV report
    Type of Medium: Series available for loan
    Pages: VII, 168 S.
    ISBN: 0858390523
    Series Statement: UNISURV report / University of New South Wales, School of Surveying S34
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
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    (Table 4) Absolute abundance of ostracoda in shallow Arctic coretop samples
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: 80PB50; 81-APB-13; AC-71-36; AC-71-38; AC-71-48; Area/locality; AW-2375; AW-2839; AW-2904; AW-2905; AW-3101A; AW-3143; AW-3154; AW-3161; AW-57-328-46; AW-62-160-10; AW-62-160-7; AW-62-160-8; AW-62-160-9; AW-IH25; AW-NN; AW-V6-33-78-21; Barnes26-80; Barnes27-80; Barnes56-80; Bart.30; Bart.46; Bart.49; Bart.55; Bart.LT23Hazel3; Bart.LT26Hazel2; Bart.LT30; Bart.LT35Hazel5; Bart.N.Omenolu; Beaufort Sea; Canadian Beaufort; Cape Martineau; Chest.Inlet1; Chest.Inlet2; Chest.Inlet5; Chest.Inlet8; Chest.Inlet9; Chikchi Sea; Counting 〉150 µm fraction; DC1-79-EG-1; DC2-80-EG-186; DC2-80-EG-73; DEPTH, sediment/rock; EGAL-75-KC-53; E Greenland; Elevation of event; Event label; Gulf of Alaska; GV8202745; GV82027-67; GV83033#44; GV83033#45; HU69-050.830; HU69-050.836; HU85-027-76; Hudson Bay; Hudson Strait; Hurd Channel; Ikerssauk15; Ikerssauk2; Ikerssauk4; Ikerssauk5; Kara Sea; Labrador; Latitude of event; Longitude of event; Melville Penin.; Northwind5; Northwind65#106; Northwind65#112; Northwind65#115; Northwind65#41; Norton Sound; N Star Bay, Greenl.; Ostracoda; Penney274101; PenneyIkerss.#1; PRZO70-22-130; PRZO72-44; Quaternary Environment of the Eurasian North; QUEEN; S5-77-BS-17; SEA5-125A; SEA-5-76-174; SW Greenland; Ungava Bay; W Greenland; WhiteBearHazel18
    Type: Dataset
    Format: text/tab-separated-values, 134 data points
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  • 3
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    Distribution of ostracoda in three long sediment cores from the deep eastern Arctic Ocean
    PANGAEA
    In:  Supplement to: Jones, Richard LI; Whatley, Robin C; Cronin, Thomas M; Dowsett, Harry J (1999): Reconstructing late Quaternary deep-water masses in the eastern Arctic Ocean using benthonic ostracoda. Marine Micropaleontology, 37(3-4), 251-272, https://doi.org/10.1016/S0377-8398(99)00022-5
    Details
    Publication Date: 2023-06-27
    Description: The distribution of Ostracoda in three long cores from the deep eastern Arctic Ocean was studied to determine the palaeoceanographical history of the Eurasian Basin during the late Quaternary. The samples for this study were obtained from the Lomonosov Ridge, Morris Jesup Rise and Yermak Plateau during the Arctic 91 expedition. Ostracoda previously studied in coretops at the same sites as the present study have shown that individual species have a strong association with different water masses and bathymetry. Throughout the late Quaternary, cores exhibit ostracod-rich layers separated by barren intervals. On the basis of biostratigraphical, isotopic and palaeomagnetic data the fossiliferous levels are interpreted as representing interglacial stages. The twenty most significant species were selected for subsequent quantitative investigation using Cluster and Factor analyses, in order to determine similarity and variance between the assemblages. An additional statistical method employing Modern Analogues and the Squared Chord Distance dissimilarity coefficient was utilised to compare the present late Quaternary fossil samples with a modern Arctic database. The results reveal a major faunal division within the Arctic Ocean Deep Water (AODW). Highly abundant and diverse assemblages within the cores were found to group and have good analogues with the Recent bathyal depth (1000-2500 m) upper AODW assemblages. Conversely, assemblages with low abundance and diversity correlate well with abyssal depth (〉3000 m) lower AODW assemblages. The palaeoceanographical history is complicated by the influence of adjacent water masses such as Canada Basin Deep Water (CBDW), Greenland Sea Deep Water (GSDW) and most importantly, Arctic Intermediate Water (AIW), which all had an influence on the ostracod assemblages during the late Quaternary. An enhanced flow of warm saline AIW into the Eurasian Basin results in species-rich upper AODW assemblages having good analogues down to 2750 m in the water column. In contrast, lower AODW assemblages influenced by cold well-oxygenated GSDW give analogues at depths as shallow as 1000 m. The faunal changes are the consequence of rapid climatic fluctuations in the eastern Arctic Ocean during the late Quaternary that are intrinsically linked to palaeoceanographical alternations in warm and cold current inflow from adjacent basins.
    Keywords: ARK-VIII/3; KAL; Kasten corer; Lomonosov Ridge, Arctic Ocean; Morris Jesup Rise; Polarstern; PS19/186; PS19/218; PS19/245; PS19 ARCTIC91; PS2185-6; PS2200-5; PS2212-3; Yermak Plateau
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 4
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    Ostracoda in surface sediments of the Arctic Ocean
    PANGAEA
    In:  Supplement to: Cronin, Thomas M; Holtz, Thomas R; Whatley, Robin C (1994): Quaternary paleoceanography of the deep Arctic Ocean based on quantitative analysis of Ostracoda. Marine Geology, 119(3-4), 305-332, https://doi.org/10.1016/0025-3227(94)90188-0
    Details
    Publication Date: 2023-06-27
    Description: Ostracodes were studied from deep Arctic Ocean cores obtained during the Arctic 91 expedition of the Polarstern to the Nansen, Amundsen and Makarov Basins, the Lomonosov Ridge, Morris Jesup Rise and Yermak Plateau, in order to investigate their distribution in Arctic Ocean deep water (AODW) and apply these data to paleoceanographic reconstruction of bottom water masses during the Quaternary. Analyses of coretop assemblages from Arctic 91 boxcores indicate the following: ostracodes are common at all depths between 1000 and 4500 m, and species distribution is strongly influenced by water mass characteristics and bathymetry; quantitative analyses comparing Eurasian and Canada Basin assemblages indicate that distinct assemblages inhabit regions east and west of the Lomonosov Ridge, a barrier especially important to species living in lower AODW; deep Eurasian Basin assemblages are more similar to those living in Greenland Sea deep water (GSDW) than those in Canada Basin deep water; two upper AODW assemblages were recognized throughout the Arctic Ocean, one living between 1000 and 1500 m, and the other, having high species diversity, at 1500-3000 m. Downcore quantitative analyses of species' abundances and the squared chord distance coefficient of similarity reveals a distinct series of abundance peaks in key indicator taxa interpreted to signify the following late Quaternary deep water history of the Eurasian Basin. During the Last Glacial Maximum (LGM), a GSDW/AODW assemblage, characteristic of cold, well oxygenated deep water 〉 3000 m today, inhabited the Lomonosov Ridge to depths as shallow as 1000 m, perhaps indicating the influence of GSDW at mid-depths in the central Arctic Ocean. During Termination 1, a period of high organic productivity associated with a strong inflowing warm North Atlantic layer occurred. During the mid-Holocene, several key faunal events indicate a period of warming and/or enhanced flow between the Canada and Eurasian Basins. A long-term record of ostracode assemblages from kastenlot core PS2200-5 (1073 m water depth) from the Morris Jesup Rise indicates a quasi-cyclic pattern of water mass changes during the last 300 kyr. Interglacial ostracode assemblages corresponding to oxygen isotope stages 1, 5, and 7 indicate rapid changes in dissolved oxygen and productivity during glacial-interglacial transitions.
    Keywords: 80PB50; 81-APB-13; AC-71-36; AC-71-38; AC-71-48; Amundsen Basin; ARK-VIII/3; AW-2375; AW-2839; AW-2904; AW-2905; AW-3101A; AW-3143; AW-3154; AW-3161; AW-57-328-46; AW-62-160-10; AW-62-160-7; AW-62-160-8; AW-62-160-9; AWI_Paleo; AW-IH25; AW-NN; AW-V6-33-78-21; Barnes26-80; Barnes27-80; Barnes56-80; Bart.30; Bart.46; Bart.49; Bart.55; Bart.LT23Hazel3; Bart.LT26Hazel2; Bart.LT30; Bart.LT35Hazel5; Bart.N.Omenolu; Beaufort Sea; Canadian Beaufort; Cape Martineau; Chest.Inlet1; Chest.Inlet2; Chest.Inlet5; Chest.Inlet8; Chest.Inlet9; Chikchi Sea; DC1-79-EG-1; DC2-80-EG-186; DC2-80-EG-73; EGAL-75-KC-53; E Greenland; Gakkel Ridge, Arctic Ocean; Giant box corer; GKG; Gulf of Alaska; GV8202745; GV82027-67; GV83033#44; GV83033#45; HU69-050.830; HU69-050.836; HU85-027-76; Hudson Bay; Hudson Strait; Hurd Channel; Ikerssauk15; Ikerssauk2; Ikerssauk4; Ikerssauk5; KAL; Kara Sea; Kasten corer; Labrador; Lomonosov Ridge, Arctic Ocean; Makarov Basin; Melville Penin.; Morris Jesup Rise; Nansen Basin; Northwind5; Northwind65#106; Northwind65#112; Northwind65#115; Northwind65#41; Norton Sound; N Star Bay, Greenl.; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Penney274101; PenneyIkerss.#1; Polarstern; PRZO70-22-130; PRZO72-44; PS19/150; PS19/151; PS19/152; PS19/155; PS19/157; PS19/158; PS19/159; PS19/160; PS19/161; PS19/164; PS19/165; PS19/166; PS19/167; PS19/171; PS19/172; PS19/173; PS19/175; PS19/176; PS19/178; PS19/181; PS19/182; PS19/183; PS19/184; PS19/185; PS19/186; PS19/189; PS19/190; PS19/192; PS19/194; PS19/198; PS19/200; PS19/204; PS19/206; PS19/210; PS19/214; PS19/218; PS19/239; PS19/241; PS19/245; PS19/246; PS19/249; PS19/252; PS19 ARCTIC91; PS2157-4; PS2158-1; PS2159-4; PS2162-1; PS2163-2; PS2164-4; PS2165-3; PS2166-2; PS2167-2; PS2168-1; PS2170-1; PS2171-1; PS2172-1; PS2174-4; PS2175-3; PS2176-4; PS2177-1; PS2178-2; PS2179-1; PS2180-1; PS2181-3; PS2182-1; PS2183-1; PS2184-1; PS2185-3; PS2186-5; PS2187-1; PS2189-1; PS2190-3; PS2192-1; PS2193-2; PS2194-1; PS2195-4; PS2196-2; PS2198-1; PS2200-2; PS2200-5; PS2209-1; PS2210-1; PS2212-5; PS2213-1; PS2214-1; PS2215-2; Quaternary Environment of the Eurasian North; QUEEN; S5-77-BS-17; SEA5-125A; SEA-5-76-174; Svalbard; SW Greenland; Ungava Bay; W Greenland; WhiteBearHazel18; Yermak Plateau
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 5
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    (Table 2) Occurrence of ostracoda in sediment core PS2200-5 (1994)
    PANGAEA
    Details
    Publication Date: 2023-07-10
    Keywords: Acetabulastoma arcticum; Argilloecia conoidea; ARK-VIII/3; AWI_Paleo; Bythoceratina scaberrima; Bythocythere sp.; Counting 〉150 µm fraction; Cytheropteron alatum; Cytheropteron bronwynae; Cytheropteron carolinae; Cytheropteron hamatum; Cytheropteron inflatum; Cytheropteron medistriatum; Cytheropteron testudo; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eucytherura complexa; Henryhowella asperrima; KAL; Kasten corer; Krithe sp.; Morris Jesup Rise; Ostracoda, other; Ostracoda indeterminata; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Paracytherois chukchiensis; Parakrithella minuta; Pedicythere neofluitans; Polarstern; Polycope sp.; PS19/218; PS19 ARCTIC91; PS2200-5; Pseudocythere caudata; Quaternary Environment of the Eurasian North; QUEEN
    Type: Dataset
    Format: text/tab-separated-values, 759 data points
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  • 6
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    (Table 2) Ostracoda abundances in sediment core PS2185-6 (Lomonosov Ridge) (1999)
    PANGAEA
    Details
    Publication Date: 2023-07-10
    Keywords: Acetabulastoma arcticum; Argilloecia conoidea; Argilloecia cylindrica; ARK-VIII/3; Bythocythere sp.; Counting; Cytheropteron bronwynae; Cytheropteron carolinae; Cytheropteron ex gr. hamatum; Cytheropteron hamatum; Cytheropteron inflatum; Cytheropteron porterae; Cytheropteron pseudoinflatum; Cytheropteron scoresbyi; Cytheropteron testudo; Cytheropteron vespertilio; DEPTH, sediment/rock; Eucythere argus; Eucytherura delineata; Henryhowella dasyderma; KAL; Kasten corer; Krithe ex gr. pernoides; Krithe glacialis; Krithe minima; Lomonosov Ridge, Arctic Ocean; Microcythere medistriatum; Ostracoda; Ostracoda, other; Paracytherois chukchiensis; Paradoxostoma sp.; Pedicythere neofluitans; Polarstern; Polycope arcys; Polycope bireticulata; Polycope bispinosa; Polycope inornata; Polycope moenia; Polycope orbicularis; Polycope punctata; Polycope semipunctata; Polycope sp.; Propontocypris trigonella; PS19/186; PS19 ARCTIC91; PS2185-6; Pseudocythere caudata; Sclerochilus contortus
    Type: Dataset
    Format: text/tab-separated-values, 532 data points
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  • 7
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    (Table 4) Ostracoda abundances in sediment core PS2212-3 (Yermak Plateau) (1999)
    PANGAEA
    Details
    Publication Date: 2023-07-10
    Keywords: Acetabulastoma arcticum; Argilloecia conoidea; Argilloecia cylindrica; ARK-VIII/3; Bythocythere sp.; Counting; Cytheropteron bronwynae; Cytheropteron carolinae; Cytheropteron ex gr. hamatum; Cytheropteron hamatum; Cytheropteron inflatum; Cytheropteron porterae; Cytheropteron pseudoinflatum; Cytheropteron scoresbyi; Cytheropteron testudo; Cytheropteron vespertilio; DEPTH, sediment/rock; Eucythere argus; Eucytherura delineata; Henryhowella dasyderma; KAL; Kasten corer; Krithe ex gr. pernoides; Krithe glacialis; Krithe minima; Microcythere medistriatum; Ostracoda; Ostracoda, other; Paracytherois chukchiensis; Paradoxostoma sp.; Pedicythere neofluitans; Polarstern; Polycope arcys; Polycope bireticulata; Polycope bispinosa; Polycope inornata; Polycope moenia; Polycope orbicularis; Polycope punctata; Polycope semipunctata; Polycope sp.; Propontocypris trigonella; PS19/245; PS19 ARCTIC91; PS2212-3; Pseudocythere caudata; Sclerochilus contortus; Yermak Plateau
    Type: Dataset
    Format: text/tab-separated-values, 836 data points
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  • 8
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    (Table 3) Ostracoda abundances in sediment core PS2200-5 (Morris Jesup Rise) (1999)
    PANGAEA
    Details
    Publication Date: 2023-07-10
    Keywords: Acetabulastoma arcticum; Argilloecia conoidea; Argilloecia cylindrica; ARK-VIII/3; Bythocythere sp.; Counting; Cytheropteron bronwynae; Cytheropteron carolinae; Cytheropteron ex gr. hamatum; Cytheropteron hamatum; Cytheropteron inflatum; Cytheropteron porterae; Cytheropteron pseudoinflatum; Cytheropteron scoresbyi; Cytheropteron testudo; Cytheropteron vespertilio; DEPTH, sediment/rock; Eucythere argus; Eucytherura delineata; Henryhowella dasyderma; KAL; Kasten corer; Krithe ex gr. pernoides; Krithe glacialis; Krithe minima; Microcythere medistriatum; Morris Jesup Rise; Ostracoda; Ostracoda, other; Paracytherois chukchiensis; Paradoxostoma sp.; Pedicythere neofluitans; Polarstern; Polycope arcys; Polycope bireticulata; Polycope bispinosa; Polycope inornata; Polycope moenia; Polycope orbicularis; Polycope punctata; Polycope semipunctata; Polycope sp.; Propontocypris trigonella; PS19/218; PS19 ARCTIC91; PS2200-5; Pseudocythere caudata; Sclerochilus contortus
    Type: Dataset
    Format: text/tab-separated-values, 2090 data points
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  • 9
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    (Table 2) Occurrence of ostracoda in surface sediments of the Arctic Ocean (1994)
    PANGAEA
    Details
    Publication Date: 2023-07-10
    Keywords: Acetabulastoma arcticum; Amundsen Basin; Argilloecia conoidea; ARK-VIII/3; AWI_Paleo; Bythoceratina scaberrima; Bythocythere sp.; Counting 〉150 µm fraction; Cytheropteron alatum; Cytheropteron bronwynae; Cytheropteron carolinae; Cytheropteron hamatum; Cytheropteron inflatum; Cytheropteron medistriatum; Cytheropteron testudo; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Eucytherura complexa; Event label; Gakkel Ridge, Arctic Ocean; Giant box corer; GKG; Henryhowella asperrima; Krithe sp.; Latitude of event; Lomonosov Ridge, Arctic Ocean; Longitude of event; Makarov Basin; Morris Jesup Rise; Nansen Basin; Ostracoda, other; Ostracoda indeterminata; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Paracytherois chukchiensis; Parakrithella minuta; Pedicythere neofluitans; Polarstern; Polycope sp.; PS19/150; PS19/151; PS19/152; PS19/155; PS19/157; PS19/158; PS19/159; PS19/160; PS19/161; PS19/164; PS19/165; PS19/166; PS19/167; PS19/171; PS19/172; PS19/173; PS19/175; PS19/176; PS19/178; PS19/181; PS19/182; PS19/183; PS19/184; PS19/185; PS19/186; PS19/189; PS19/190; PS19/192; PS19/194; PS19/198; PS19/200; PS19/204; PS19/206; PS19/210; PS19/214; PS19/218; PS19/239; PS19/241; PS19/245; PS19/246; PS19/249; PS19/252; PS19 ARCTIC91; PS2157-4; PS2158-1; PS2159-4; PS2162-1; PS2163-2; PS2164-4; PS2165-3; PS2166-2; PS2167-2; PS2168-1; PS2170-1; PS2171-1; PS2172-1; PS2174-4; PS2175-3; PS2176-4; PS2177-1; PS2178-2; PS2179-1; PS2180-1; PS2181-3; PS2182-1; PS2183-1; PS2184-1; PS2185-3; PS2186-5; PS2187-1; PS2189-1; PS2190-3; PS2192-1; PS2193-2; PS2194-1; PS2195-4; PS2196-2; PS2198-1; PS2200-2; PS2209-1; PS2210-1; PS2212-5; PS2213-1; PS2214-1; PS2215-2; Pseudocythere caudata; Quaternary Environment of the Eurasian North; QUEEN; Svalbard; Yermak Plateau
    Type: Dataset
    Format: text/tab-separated-values, 2553 data points
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  • 10
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    Petrology and geochemistry of basalts from the Vavilov Basin (1990)
    PANGAEA
    In:  Supplement to: Bertrand, Herve; Boivin, P; Robin, C (1990): Petrology and geochemistry of basalts from the Vavilov Basin (Tyrrhenian Sea), Ocean Drilling Program Leg 107, Holes 651A and 655B. In: Kastens, KA; Mascle, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 107, 75-92, https://doi.org/10.2973/odp.proc.sr.107.142.1990
    Details
    Publication Date: 2024-01-09
    Description: During ODP Leg 107, two holes were drilled in the basement of Vavilov Basin, a central oceanic area of the Tyrrhenian sea. Hole 655B is located near the Gortani ridge in off-axis position at the western rim of the basin; Hole 651A is located on a basement swell at the axis of the basin. This paper deals with mineral chemistry, major and trace element geochemistry, and petrogenesis of the basalts recovered in the two holes. The mineralogy of the basalts is broadly homogeneous, but all of them have suffered important seawater alteration. Their major-element compositions are similar to both normal-mid-ocean-ridge-basalts (N-MORB) and back-arc-basalts (BAB) except for Na2O contents (BAB-like), and K2O which is somewhat enriched in upper unit of Hole 651 A. Their affinity with N-MORB and BAB is confirmed by using immobile trace elements such as Zr, Y, and Nb. However, basalts from the two sites present contrasting geochemical characteristics on spidergrams using incompatible elements. Hole 655B basalts are homogeneous enriched tholeiites, similar to those from DSDP Hole 373 (located on the opposite side of the basin near the eastern rim), and show affinities with enriched MORB (E-MORB). At Hole 651 A, the two basalt units are chemically distinct. One sample recovered in lower unit is rather similar to those from Hole 655B, but basalts from upper unit display calc-alkaline characteristic evidenced by the increase of light-ion-lithophile-element (LILE)/high-field-strength-element (HFSE) ratio, and appearance of a negative Nb-anomaly, making them comparable with orogenic lavas from the adjacent Eolian arc. The observed chemical compositions of the basalts are consistent with a derivation of the magmas from a N-MORB type source progressively contaminated by LILE-enriched fluids released from dehydration of the bordering subducted plate. Implications for evolution of the Tyrrhenian basin are tentatively proposed taking into consideration geochemical and chronological relationships between basalts from Leg 107 Holes 655B and 651 A, together with data from Leg 42 Site 373 and Vavilov Seamount. These data illustrate back-arc spreading in ensialic basin closely associated with the maturation of the adjacent subduction, followed by the growth of late off-axis central volcano, whereas the active subduction retreats southeastward.
    Keywords: 107-651A; 107-655B; DRILL; Drilling/drill rig; Joides Resolution; Leg107; Ocean Drilling Program; ODP; Tirreno Sea
    Type: Dataset
    Format: application/zip, 8 datasets
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