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
id doaj-39b1a895630844949e520957c7c1da88
record_format Article
spelling doaj-39b1a895630844949e520957c7c1da882020-11-25T00:29:29ZengGeological AgencyIndonesian Journal on Geoscience2355-93142355-93062014-06-015211311810.17014/ijog.5.2.113-11896Tren kenaikan suhu permukaan laut pada abad ke-14 berdasarkan data geokimia Sr/Ca dari fosil koral MentawaiSri Y. Cahyarini0Puslit Geoteknologi LIPI, Kompleks LIPI Gd. 70 Sangkuriang Bandung<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>https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/96coralSr/Casea surface temperature
collection DOAJ
language English
format Article
sources DOAJ
author Sri Y. Cahyarini
spellingShingle Sri Y. Cahyarini
Tren kenaikan suhu permukaan laut pada abad ke-14 berdasarkan data geokimia Sr/Ca dari fosil koral Mentawai
Indonesian Journal on Geoscience
coral
Sr/Ca
sea surface temperature
author_facet Sri Y. Cahyarini
author_sort Sri Y. Cahyarini
title Tren kenaikan suhu permukaan laut pada abad ke-14 berdasarkan data geokimia Sr/Ca dari fosil koral Mentawai
title_short Tren kenaikan suhu permukaan laut pada abad ke-14 berdasarkan data geokimia Sr/Ca dari fosil koral Mentawai
title_full Tren kenaikan suhu permukaan laut pada abad ke-14 berdasarkan data geokimia Sr/Ca dari fosil koral Mentawai
title_fullStr Tren kenaikan suhu permukaan laut pada abad ke-14 berdasarkan data geokimia Sr/Ca dari fosil koral Mentawai
title_full_unstemmed Tren kenaikan suhu permukaan laut pada abad ke-14 berdasarkan data geokimia Sr/Ca dari fosil koral Mentawai
title_sort tren kenaikan suhu permukaan laut pada abad ke-14 berdasarkan data geokimia sr/ca dari fosil koral mentawai
publisher Geological Agency
series Indonesian Journal on Geoscience
issn 2355-9314
2355-9306
publishDate 2014-06-01
description <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>
topic coral
Sr/Ca
sea surface temperature
url https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/96
work_keys_str_mv AT sriycahyarini trenkenaikansuhupermukaanlautpadaabadke14berdasarkandatageokimiasrcadarifosilkoralmentawai
_version_ 1725330916832706560