Present address: Schlumberger, DCS Well Placement, Risabergveien 3, N-4056 Tananger, Norway.
Carbonate facies patterns in surface sediments of upwelling and non-upwelling shelf environments (Panama, East Pacific)
Article first published online: 24 FEB 2011
© 2010 The Authors. Journal compilation © 2010 International Association of Sedimentologists
Special Issue: Carbonate platforms: archives of past global change Special Issue
Volume 59, Issue 1, pages 32–56, January 2012
How to Cite
REIJMER, J. J. G., BAUCH, T. and SCHÄFER, P. (2012), Carbonate facies patterns in surface sediments of upwelling and non-upwelling shelf environments (Panama, East Pacific). Sedimentology, 59: 32–56. doi: 10.1111/j.1365-3091.2010.01214.x
- Issue published online: 19 DEC 2011
- Article first published online: 24 FEB 2011
- Manuscript received 05 August 2010; revision accepted 03 November 2010
- Carbonate sedimentation;
- Eastern Pacific;
- facies patterns;
In this study two carbonate environments are compared and contrasted; the Gulf of Panama and the Gulf of Chiriquí on the Pacific side of Panama. These two embayments are in close geographic proximity at latitudes between 7° N and 9° N. The Gulf of Panama and the Gulf of Chiriquí are characterized by contrasting oceanographic conditions with year-round stable non-upwelling conditions in the Gulf of Chiriquí and strong seasonal upwelling in the dry season (December to April) in the Gulf of Panama. The upwelling variations only have a limited influence on the amount of carbonate produced; however, they do have a major impact on the occurrence of specific carbonate producing biota. In addition, carbonate production and distribution is influenced in both gulfs by the occurrence of islands and by terrigenous input. Terrigenous material is found mainly in the smaller grain sizes (<63 to 250 μm) that can be transported easily by currents and waves. Carbonate dominant sediments (carbonate sands and mixed carbonate–siliciclastic sands) mainly occur around the islands and are dominated by larger grain-sizes (>500 μm). The Gulf of Panama and the Gulf of Chiriquí both show warm and temperate carbonate-producing biota, with carbonate producers from tropical (corals) to mixed tropical to cool-water (coralline red algae) and cold-water (balanids) environments. The Gulf of Chiriquí is characterized by oligotrophic to mesotrophic conditions resulting in a photozoan (coral) and/or rhodolith-facies in shallow-water areas surrounding the islands and a mollusc-dominated facies in deeper waters towards the shelf edge. Seasonal upwelling causes temporary eutrophic conditions in the Gulf of Panama, which results in a heterozoan facies around the islands dominated by balanids, echinoderms and molluscs. Thus a ‘cool-water’ carbonate fauna and eutrophic conditions can exist in the tropics within an area prone to seasonal upwelling. The distinct facies differences found on the Pacific shelf of Panama stress the importance of variations in oceanographic conditions, upwelling versus non-upwelling, in determining carbonate production and associated facies patterns in the tropics.