Tren kenaikan suhu permukaan laut pada abad ke-14 berdasarkan data geokimia Sr/Ca dari fosil koral Mentawai

<p>DOI: <span><a href="http://dx.doi.org/10.17014/ijog.v5i2.96" target="_blank">10.17014/ijog.v5i2.96</a></span></p><p>Sr/Ca content ratio in coral is a promising tool for a sea surface temperature reconstruction. In this study, Sr/Ca was...

Full description

Bibliographic Details
Main Author: Sri Y. Cahyarini
Format: Article
Language:English
Published: Geological Agency 2014-06-01
Series:Indonesian Journal on Geoscience
Subjects:
Online Access:https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/96
Description
Summary:<p>DOI: <span><a href="http://dx.doi.org/10.17014/ijog.v5i2.96" target="_blank">10.17014/ijog.v5i2.96</a></span></p><p>Sr/Ca content ratio in coral is a promising tool for a sea surface temperature reconstruction. In this study, Sr/Ca was analyzed from the top core of fossil coral from Central Mentawai, Indonesia (BLS). The dating of U/Th is used for the age determination of the fossil coral. Based on the U/Th dating, the fossil coral used in this study was deposited in 14th century which approximately has a time range 11 years. The result of this study shows that in the 14th century, the sea surface temperature increased by 3.20 C during 11 years period.<br /><br /></p>
ISSN:2355-9314
2355-9306