--> ABSTRACT: Otoliths of the Late Miocene Gatun Formation of Panama, by R. L. Martin and D. A. Dunn; #90908 (2000)

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ABSTRACT: Otoliths of the Late Miocene Gatun Formation of Panama

MARTIN, ROBERT L., West Virginia University, Morgantown, WV; and DEAN A. DUNN, Univ. Southern Mississippi, Hattiesburg, MS 39406-5044

The Gatun Formation is a Late Miocene tuffaceous litharenite (volcanic sandstone) that is exposed on the north side of Lake Gatun, and is cut by the Panama Canal. This formation contains molluscs indicating a shallow nearshore environment, and it has been age-dated by its planktonic foraminifera (Zones N14-N17) and calcareous nannofossils (Zones NN10-NN11).

Examination of Gatun samples collected just east of Cativa, Colon Province, Panama, reveals abundant fish otoliths. Otoliths are the aragonitic elements within the otic capsule of fishes, which allow them to hear and to orient themselves in the water column. Because of their durability, otoliths are often used in paleobathymetric analyses.

The otolith assemblage is dominated by Gobiids, Lutjanids, Bothids, Sciaenids, Engraulids, Haemulids, Cynoglossids, and Batrachoidids. Myctophids are less common, but are present in relatively substantial numbers.

The dominance of neritic Gobiids supports the interpretation of deposition in a shallow nearshore environment, with Haemulids indicating a sandy substrate. Cyaenids are found in modern euryhaline environments. The presence of Myctophids and the absence of Macrourids indicate some oceanic influence.

No otolith taxon found was exclusively, Pacific, and most taxa are restricted to, or more diverse in, the Atlantic Ocean, indicating a close affinity to the assemblages of the modern Gulf of Mexico.

MARTIN, ROBERT L., and DEAN A. DUNN

 

AAPG Search and Discovery Article #90908©2000 GCAGS, Houston, Texas