Recent Outer-Shelf Foraminiferal Assemblages on the Carnarvon Ramp and Northwestern Shelf of Western Australia

• Main Authors: Haller, Christian, Hallock, Pamela, Hine, Albert C., Smith, Christopher G.
• Format: Conference Object
• Language: unknown
• Published: Digital Commons @ University of South Florida 2019
• Subjects: Life Sciences; Indian; Pacific; Planktonic foraminifera
• Online Access: https://digitalcommons.usf.edu/msc_facpub/1210; https://doi.org/10.2110/sepmsp.111.05; https://sedimentary-geology-store.com/catalog/book/geologic-problem-solving-microfossils-iv

The carbonate sediments of the Western Australian shelf in the Indian Ocean host diverse assemblages of benthic foraminifera. These shelf environments are dominated by the southward-flowing Leeuwin Current, which impacts near-surface circulation and influences biogeographic ranges of Indo-Pacific warm-water foraminifera. Analyses of outer-ramp to upper-slope sediments (127-264 m water depth) at four different sites (some with replicates) revealed 185 benthic species. A shift from benthic to planktonic foraminifera was accompanied by a decrease in ''larger'' benthic foraminifera below the lowermost euphotic zone. Fisher a and proportions of buliminid and textulariid taxa increased with water depth, as miliolids and rotaliids decreased in proportion. Cluster analyses on the 125 to 250 lm and 250 to 850 lm size fractions revealed distinct assemblages, with the former distinguishing between deeper and shallower sites, and the latter distinguishing between the Carnarvon Ramp site and the three sites on the northwestern shelf (NWS). The assemblage shift with depth was likely caused by rapidly changing physical conditions in the upper thermocline. The assemblage differences between the NWS and the Carnarvon Ramp site indicate limited horizontal transport and migration rates on the outer shelf below the influence of the Leeuwin Current. Similarity in bottom-water temperature at the studied sites indicates that water mass characteristics, biogeographic history, and/or possibly diversity in benthic shelf habitats, rather than temperature and depth, are responsible for differences between the two regions.