T138 Applying Near Surface Geophysics to Solve Geological Problems

Wednesday, 28 October 2020
1:30 PM - 5:30 PM
Meeting Rooms

ELLIPTICITY OF TEKTITE-LIKE, HIGH SIO2 SPHERULES FROM THE ROSS SEA

Paper number: T138-14
Program: Technical Sessions
Time: 4:20 PM – 4:30 PM

Authors

Abstract

High SiO2 spherules have been found in abundance in Antarctic Ross Sea cores at subbottom depths of 10 to 800 cm. Their morphology is variable, ranging from round to ovoid. Many spherules resemble tektites, featuring aerodynamic shapes, such as dumbbells and spheroids with short tails [1]. However, many Ross Sea spherules display characteristics that have not been observed in tektites, including pimpled surfaces and long tails. While these spherules are often >90% SiO2, they are composed of alternating layers of C and SiO2, and these layers often exfoliate along their contact surface. Additionally, many Ross Sea spherules feature long ablation tracks on their surfaces. Some researchers have proposed a cyclic model of formation for Ross Sea spherules, wherein seasonal ice melts increase salinity of the Ross Sea, leading to greater silica precipitation [2]. Others have proposed a biological origin [3]. These hypotheses are unsatisfying, as the aerodynamic shapes observed in Ross Sea Spherules would not be produced by simple precipitation. Moreover, neither the geochemical composition nor new SEM images are indicative of a biological origin. Ross Sea Core NBP9501-39KC has been previously dated [4]. The age model for this core indicates an age of circa 10-13 ka BP. Sixty-eight Orbulina Universa were picked and digitally analyzed against 89 Ross Sea Spherules for ellipticity. Ross Sea Spherules are morphologically distinct (ellipticity of 0.201 ± 0.027) from Orbulina Universa (ellipticity of .068 ± .006), precluding a biological mechanism of formation.

[1] O'Keefe, John Aloysius. 1976. “Tektites and Their Origin.” Netherlands: Elsevier Scientific Publishing Company.

[2] Perry, Pamela. 1999. “Quaternary Benthic Foraminiferal Distribution in the Ross Sea, Antarctica, and Its Relationship to Oceanography.” Louisiana State University.

[3] Weiterman, SD and Russell, MD. 1986. “Siliceous ooids from antarctic marine sediments.” Antarctic Journal of the United States, Volume 21, Issues 1-5. Pp. 159.

[4] Cunningham, W. L., Leventer, A., Andrews, J. T., Jennings, A. E., and Licht, K. J., 1999. "Late Pleistocene-Holocene marine conditions in the Ross Sea, Antarctica: evidence from the diatom record." The Holocene, v. 9, p. 129-139.

Geological Society of America Abstracts with Programs. Vol. 52, No. 6

doi: 10.1130/abs/2020AM-358357

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