2009•Unpublished venueRequires access

Paleoclimate Reconstruction Based on Oxygen Isotope Composition of Foraminifera in Southern Mountains Area, Central Java -Indonesia

Akmaluddin Akmaluddin

Abstract

The planktonic foraminifera (Orbulina universa and Globigerinoides sacculifer) and benthic foraminifera (Cibicidoides, Uvigerina and Nodosari) taken from Southern Mountains (Sambipitu Fm., Oyo Fm and Kepek Fm.) were collected for measuring the oxygen isotope. The purpose of this research is trying to calculate the composition of the oxygen isotope from the foraminifera for reconstructing the paleoclimate. The preliminary result of the samples taken from Sambipitu and Oyo Formations shows that the isotope values are

About this research paper

What this paper is about

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Key concepts: Foraminifera, Globigerinoides, Geology, Isotopes of oxygen, Paleoclimatology, Oceanography, Benthic zone, Micropaleontology