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GeoRef Categories
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Availability
IN MEMORY OF BRENT WILSON B.SC. (HONS), M.SC., PH.D. (1959–2024) Open Access
AN INTEGRATED APPROACH TO ENVIRONMENTAL HEALTH ASSESSMENT OF A CORAL REEF ECOSYSTEM BASED UPON FORAMINIFERA Open Access
IN MEMORY OF DR. SILVIA SPEZZAFERRI, PHD, MER (1961–2024) Open Access
Why Amphistegina lobifera , a tropical benthic foraminiferal species, is thriving at temperate latitudes in the Mediterranean Sea Open Access
In Memory of Prof. Dr. Ercan Özcan Open Access
Benthic Foraminiferal Dynamics in Reef-Associated Sediments of Jobos Bay, Puerto Rico: 2018–2019 Open Access
Distribution and Diversity of Benthic Foraminifera in the Coastal Area of Al-Bawadi Island, Southern Red Sea Available to Purchase
Can Areas of High Alkalinity Freshwater Discharge Provide Potential Refugia for Marine Calcifying Organisms? Available to Purchase
Growth and Fecundity of Marginopora Vertebralis and Amphistegina Lobifera in Laboratory Culture Available to Purchase
Microbial Associations of Four Species of Algal Symbiont-bearing Foraminifers from the Florida Reef Tract, Usa Available to Purchase
Distribution of Modern Salt-marsh Foraminifera from the Eastern Mississippi Sound, U.s.a. Available to Purchase
RECENT OUTER-SHELF FORAMINIFERAL ASSEMBLAGES ON THE CARNARVON RAMP AND NORTHWESTERN SHELF OF WESTERN AUSTRALIA Available to Purchase
Abstract: 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 α 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 μm and 250 to 850 μm 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.