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The enigma of rare Quaternary oolites in the Indian and Pacific Oceans: A result of global oceanographic physicochemical conditions or a sampling bias?

Lookup NU author(s): Benjamin Petrick

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Abstract

© 2018 Elsevier Ltd Marine ooids are iconic indicators of shallow seawater carbonate saturation state, and their formation has traditionally been ascribed to physicochemical processes. The Indo-Pacific stands out as a region devoid of oolites, particularly during the Quaternary: the “ooid enigma”. Here we present results from recent coring by the International Ocean Discovery Program (IODP Expedition 356) off west Australia that shows that ooid horizons are common in Pleistocene strata up to 730,000 years old. Extensive “ooid factories” were created due to the presence of long-lived tidally influenced flat–topped tropical platforms suitable for intermittent ooid accretion over hundreds to thousands of years during highstands and times of lower sea level. This work suggests marine ooids may actually be more common in Indo-Pacific than previously reported. Past global ocean alkalinity was elevated during Pleistocene glacial periods and continental climate was generally more arid in the Indo-Pacific region compared to interglacials and the Holocene. Therefore, increased aridity associated with higher alkalinity conditions during the glacials facilitated ooid precipitation on adjacent tropical carbonate platforms particularly offshore from arid Australia. This confluence of factors suggests that more “ooid factories” may be encountered by further coring Indo-Pacific regions with Pleistocene flat long-lived carbonate shelves. However, Indo-Pacific Quaternary ooid occurrences outside Australia are rare, suggesting that the Northwest Shelf may be a unique archive of this non-skeletal precipitate. Further investigations into the petrography and geochemistry of pre-Holocene ooid occurrences will provide insights into their origin and the relative role of biotic, physicochemical and other factors in their formation.


Publication metadata

Author(s): Gallagher SJ, Reuning L, Himmler T, Henderiks J, De Vleeschouwer D, Groeneveld J, Rastigar Lari A, Fulthorpe CS, Bogus K, Renema W, McGregor HV, Kominz MA, Auer G, Baranwal S, Castaneda S, Christensen BA, Franco DR, Gurnis M, Haller C, He Y, Ishiwa T, Iwatani H, Jatiningrum RS, Korpanty CA, Lee EY, Levin E, Mamo BL, McHugh CM, Petrick BF, Potts DC, Takayanagi H, Zhang W

Publication type: Article

Publication status: Published

Journal: Quaternary Science Reviews

Year: 2018

Volume: 200

Pages: 114-122

Online publication date: 08/10/2018

Acceptance date: 18/09/2018

ISSN (print): 0277-3791

ISSN (electronic): 1873-457X

Publisher: Elsevier Ltd

URL: https://doi.org/10.1016/j.quascirev.2018.09.028

DOI: 10.1016/j.quascirev.2018.09.028


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