ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • AGE; Assilina ammonoides; Asterorotalia concinna; Asterorotalia gaimardii; Asterorotalia milletti; Asterorotalia sp.; Austin-1; Bounty-1; Counting; Counting, foraminifera, benthic; DEPTH, sediment/rock; Event label; Foraminifera; Foraminifera, benthic; Foraminifera, per unit sediment mass; Goodwyn-6; Goodwyn-7; Heterolepa margaritifera; Maitland-1; Matiland_North-1; North west Australian continental margin; Nummulites venosa; Plankton; Pseudorotalia angusta; Pseudorotalia globosa; Pseudorotalia indopacifica; Pseudorotalia schroeteriana; Tryal_Rocks-1; West_Tryal_Rocks-1  (1)
  • GEOPHYSICS  (1)
Collection
Keywords
Publisher
Years
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Gallagher, Stephen John; Wallace, Malcolm W; Li, Chung Leong; Kinna, Belinda; Bye, John A T; Akimoto, Kazumi; Torii, Masayuki (2009): Neogene history of the West Pacific Warm Pool, Kuroshio and Leeuwin currents. Paleoceanography, 24, PA1206, https://doi.org/10.1029/2008PA001660
    Publication Date: 2023-05-12
    Description: Foraminiferal analysis of Miocene to recent strata of the Northwest Shelf of Australia is used to chart West Pacific Warm Pool (WPWP) influence. The assemblage is typified by "larger" foraminifera with ingressions of the Indo-Pacific "smaller" taxa Asterorotalia and Pseudorotalia at around 4 Ma and from 1.6 to 0.8 Ma. A review of recent and fossil biogeography of these taxa suggests their stratigraphic distribution can be used to document WPWP evolution. From 10 to 4.4 Ma a lack of biogeographic connectivity between the Pacific and Indian Ocean suggests Indonesian Throughflow (ITF) restriction. During this period, the collision of Australia and Asia trapped warmer waters in the Pacific, creating a central WPWP biogeographic province from the equator to 26°N. By 3 Ma Indo-Pacific species migrated to Japan with the initiation of the "modern" Kuroshio Current coinciding with the intensification of the North Pacific Gyre and Northern Hemisphere ice sheet expansion. Indo-Pacific taxa migrated to the northwest Australia from 4.4 to 4 Ma possibly because of limited ITF. The absence of Indo-Pacific taxa in northwest Australia indicates possible ITF restriction from 4 to 1.6 Ma. Full northwest Australian biogeographic connectivity with the WPWP from 1.6 to 0.8 Ma suggests an unrestricted stronger ITF (compared to today) and the initiation of the modern Leeuwin Current. The extinction of some Indo-Pacific species in northwest Australia after 0.8 Ma may be related to the effects of large glacial/interglacial oscillations and uplift of the Indonesian Archipelago causing Indonesian seaway restriction.
    Keywords: AGE; Assilina ammonoides; Asterorotalia concinna; Asterorotalia gaimardii; Asterorotalia milletti; Asterorotalia sp.; Austin-1; Bounty-1; Counting; Counting, foraminifera, benthic; DEPTH, sediment/rock; Event label; Foraminifera; Foraminifera, benthic; Foraminifera, per unit sediment mass; Goodwyn-6; Goodwyn-7; Heterolepa margaritifera; Maitland-1; Matiland_North-1; North west Australian continental margin; Nummulites venosa; Plankton; Pseudorotalia angusta; Pseudorotalia globosa; Pseudorotalia indopacifica; Pseudorotalia schroeteriana; Tryal_Rocks-1; West_Tryal_Rocks-1
    Type: Dataset
    Format: text/tab-separated-values, 1254 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2013-08-31
    Description: Geochemical investigations on the widely dispersed Late Proterozoic Acraman impact ejecta horizon and its host marine shales in the Adelaide Geosyncline provide strong evidence for low-temperature mobilization of the platinum group elements (PGE), including Ir. The ejecta horizon was formed when the middle Proterozoic dacitic volcanics in the Gawler Ranges, central South Australia, were impacted by a very large (ca. 4 km) meteorite. The resulting structure, now represented by Lake Acraman, is Australia's largest meteorite impact structure. Debris from the impact was blasted for many hundreds of kilometers, some falling into the shallow sea of the Adelaide Geosyncline, some 300 km to the east of the impact site.
    Keywords: GEOPHYSICS
    Type: Lunar and Planetary Inst., International Conference on Large Meteorite Impacts and Planetary Evolution; p 23
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...