Sightings of the Rare Globorotalia Cavernula in the Subantarctic South of Africa: Biogeochemical and Ecological Insights

Author:

Smart Sandi M.12,Schiebel Ralf2,Jochum Klaus P.2,Chaabane Sonia234,Jentzen Anna2,Repschläger Janne2,Stoll Brigitte2,Weis Ulrike2,Haug Gerald H.2

Affiliation:

1. 1 Department of Geological Sciences, The University of Alabama, Box 870338, Tuscaloosa, AL 35487, USA

2. 2 Climate Geochemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany

3. 3 CEREGE, Technopôle Environnement Arbois Méditerranée, Avenue Louis Philibert, BP80, 13545 Aix en Provence, Cedex 04, France

4. 4 FRB-Cesab, Institut Bouisson Bertrand, 5 rue de l’École de Médecine, 34000 Montpellier, France

Abstract

Abstract Over 50 years since its discovery and decades since its last recorded sighting in the modern ocean, Globorotalia cavernula has made another appearance: now in Subantarctic plankton tows south of Africa. This finding expands the known modern range of the species, which was commonly thought to be absent from the Atlantic sector of the Southern Ocean. Here, we use high-resolution microscopy and trace element analysis (fs-LA-ICP-MS) as a window into the ecology and habitat of this enigmatic species. Shell-averaged trace element ratios of G. cavernula are consistent with the cool–cold, well-oxygenated, open-ocean waters where it was collected (low Mg/Ca, Mn/Ca); and Sr/Ca is the least variable. Chamber-to-chamber trends are generally similar to other non-spinose species, but absolute values (e.g., Ba/Ca) can differ substantially. Combining our data with previous sightings suggests under-sampling/under-reporting of G. cavernula in the modern/recent Southern Ocean, and possibly an expanded geographic range during the colder Pleistocene Epoch.

Publisher

Cushman Foundation for Foraminiferal Research

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