Fossil otoliths, from the Gulf of Kutch, Western India, as a paleo-archive for the mid- to late-Holocene environment

被引：13
|
作者：
Amekawa, Shota [1 ,2 ]
Kubota, Kaoru [1 ,2 ]
Miyairi, Yosuke [1 ]
Seki, Arisa [1 ,2 ]
Kawakubo, Yuta [1 ,2 ]
Sakai, Saburo [3 ]
Ajithprasad, P. [4 ]
Maemoku, Hideaki [5 ]
Osada, Toshiki [6 ]
Yokoyama, Yusuke [1 ,2 ,3 ]
机构：
[1] Univ Tokyo, Analyt Ctr Environm Study, Atmosphere & Ocean Res Inst, 5-1-5 Kashiwanoha, Kashiwa, Chiba 2778564, Japan
[2] Univ Tokyo, Grad Sch Sci, Dept Earth & Planetary Sci, 7-3-1 Hongo, Tokyo 1130033, Japan
[3] Japan Agcy Marine Earth Sci & Technol, Dept Biogeosci, 2-15 Natsushima Cho, Yokosuka, Kanagawa 2370061, Japan
[4] Maharaja Sayajirao Univ Baroda, Dept Archaeol & Ancient Hist, Vadodara 390002, Gujarat, India
[5] Hosei Univ, Dept Geog, 2-17-1 Fujimi, Tokyo 1028160, Japan
[6] Natl Inst Humanities, Res Inst Humanity & Nat, Kita Ku, 457-4 Motoyama, Kyoto 6038047, Japan
来源：
QUATERNARY INTERNATIONAL | 2016年 / 397卷
关键词：
Otolith; Monsoon; Mid Holocene; 4.2 ka event; LA-ICPMS; ISOTOPE FRACTIONATION; SUMMER MONSOON; SEA-LEVEL; OXYGEN; CARBON; TEMPERATURE; MARINE; FISH; VARIABILITY; STRONTIUM;
D O I：
10.1016/j.quaint.2015.07.006
中图分类号：
P9 [自然地理学];
学科分类号：
0705 ; 070501 ;
摘要：
Abundantly available catfish otoliths excavated from the ruins of the Indus civilization, in the coastal regions of Western India, are expected to preserve a detailed paleoclimatological record of the mid-to late-Holocene. In this study, we analyzed saltwater catfish otoliths recovered from the Gulf of Kutch, Western India. Stable isotopes (oxygen and carbon) and elemental ratios (Ba/Ca and Sr/Ca) were measured by isotope ratio mass spectrometry (IRMS) and high-resolution laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS), respectively. Oxygen isotopes of a modern otolith (delta O-18) indicates the interval when the catfish would have dwelt in the sea and appear to record seasonal temperature variability with a precision of 1 C degrees. Calculated temperatures from delta O-18 of a fossil otolith dated to 4.3 cal ka BP indicates that the minimum temperature in winter was similar to 2.5 C degrees lower than that of the present. Although comparison to alkenone results from the northwestern Arabian Sea indicates potential temperature underestimation, further measurements of modern and fossil samples would lead to more precise reconstruction of temperature history during mid- to late-Holocene. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
引用
收藏
页码：281 / 288
页数：8
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