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ABSTRACT ONLY

 

STEGODON FOSSIL REMAINS FROM THE PLIO-PLEISTOCENE
LAGUNA FORMATION, ANTIPOLO, RIZAL, PHILIPPINES
 


WALTER V. SCHOELL. PRISCILLA J.
MILITANTE-MATIAS AND ALYSSA M. PELEO

National Institute of Geological Sciences (NIGS)
College of Science, University of the Philippines (U.P.)
Diliman, Quezon City. Philippines

Dr. Walter U. Schoell, Visiting Professor of Geology, NIGS, U.P.
Dr. Priscilla J. Militante-Matias, Professor of Geology
Ms. Alyssa M. Peleo, Univ. Research Associate I, NIGS, U.P.


 

 

 

 

ABSTRACT


In the Tres Hermanas Area, Antipolo, Rizal, Philippines, the Plio-Pleistocene Laguna Formation is made up mainly of tuffs deposited in an alluvial setting. The formation exhibits cycles of extensive tuff deposition interrupted by periods of soil development shown by paleosol horizons intensively colonized by plant growth. Stegodon fossil remains consist of teeth, tusk and bone pieces belonging to at least 5 different animals that have been unearthed from the area. The fossil specimens and paleobotanical data indicate a subtropical moderate climate. lt is suggested that the proboscideans reached the Philippine Islands eventually by non continuous land bridges where the animals had to cross and swim through salt water barriers.
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