Establishment of utility ranking for fossil datum planes in Upper Cretaceous sequences based on carbon isotope stratigraphy.
基于碳同位素地层学的上白垩统化石基准面效用排序的建立
基本信息
- 批准号:13640469
- 负责人:
- 金额:$ 2.18万
- 依托单位:
- 依托单位国家:日本
- 项目类别:Grant-in-Aid for Scientific Research (C)
- 财政年份:2001
- 资助国家:日本
- 起止时间:2001 至 2003
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
(1)About two kilometers of detailed plan map(1/1000) along Horotate River in Kotanbetsu, Tomamae Town, Hokkaido, Japan was drawn based on measurement and careful investigation of macro fossil occurrences. Plan maps in 1/5000 scale were also made in the Oyubari, Hobetsu and Haboro areas. Mudstone samples were collected during the survey and the localities are indicated within these plan maps.(2)Along Horotate River, macrofossil did not show abundant occurrences, however, continuous occurrence of regionally important age indicative species, namely Inoceramus hobetsensis, was identified. It enabled us to delimit the stratigraphic distribution of this species in detail.(3)Carbon isotope analysis on majority of samples from Horotate River sequence have been suspended because of machine troubles at an institute where we have expected to analyze them. Samples from Oyubari and Hobetsu areas and a part of samples from Horotate River sequence were analyzed at Indiana University, U.S.A.Each carbon isotope profile for each area showed internationally recognizable pattern that enables us to calibrate biohorizons of macrofossil within the framework of international correlation.(4)Planktonic foraminifers from Hobetsu area include variety of age indicative species. Among them, continuous occurrence of Helvetoglobotruncana helvetica addresses stratigraphic range of internationally significant foraminiferal zone. Four other cosmopolitan species also support stratigraphic position of upper limit of H.helvetica Zone in this area.(5)Continuous effort for establishment of detailed chronostratigraphy for the Cretaceous in Hokkaido will be carried out after this project. Such data collection will open the way for utilizing the Yezo Group as an international chronological standard succession.
(1)通过对大型化石产状的测量和仔细调查,绘制了日本北海道Tomamae町Kotanbetsu的沿着Horotate川约2公里的详细平面图(1/1000)。还在大夕张、霍别和哈博罗地区绘制了1/5000比例的平面图。在调查期间采集了泥岩样本,并在这些平面图中注明了地点。(2)在沿着Horotate河沿岸,大型化石没有显示出丰富的产出,但鉴定出区域重要的年龄指示种Inoceramus hobetsensis的连续出现。它使我们能够详细地划定本种的地层分布。(3)由于我们希望分析的一个研究所的机器故障,对Horotate河序列中大部分样品的碳同位素分析已经暂停。在美国印第安纳州大学对大夕张和保别地区的样品以及部分Horotate River层序样品进行了分析。(4)保别地区浮游有孔虫包括多种年龄指示种。其中,Helvetoglobotruncana helvetica的连续出现解决了国际重要有孔虫带的地层范围。另外四种广布种也支持了该地区H.helvetica带上限的地层位置。(5)本项目结束后,将继续努力建立北海道白垩纪的详细年代地层。这种数据收集将为利用Yezo集团作为国际时间顺序标准继承开辟道路。
项目成果
期刊论文数量(12)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
土屋 健, 長谷川 卓, リサM.プラット: "北海道蝦夷層群における炭素同位体比曲線とイノセラムス生層序の対応関係"地質学雑誌. 109. 30-40 (2003)
Ken Tsuchiya、Takashi Hasekawa、Lisa M. Pratt:“北海道虾夷群碳同位素比值曲线与 Inoceramus 生物地层学的对应关系”地质杂志 109. 30-40 (2003)。
- DOI:
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- 影响因子:0
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- 通讯作者:
Hirano, H., Sakai, T., Hayakawa, H., Saiki, K., Hasegawa, T., Kano, M., Hikida, Y., Takahashi, K., Kawabe, F.: "Eenvironments of the Cretaceous Yezo forearc basin --carbon cycle and bio-diversity change--."Bulletin of Nakagawa Museum of Natural History(no
Hirano, H.、Sakai, T.、Hayakawa, H.、Saiki, K.、Hasekawa, T.、Kano, M.、Hikida, Y.、Takahashi, K.、Kawabe, F.:“白垩纪的环境
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- 影响因子:0
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Hasegawa, T.: "A global carbon-isotope event in the Middle Turonian(Cretaceous) sequences in Japan and Russian Far East."Proceedings of Japan Academy Series B. vol.79. 141-144 (2003)
Hasekawa, T.:“日本和俄罗斯远东中土仑阶(白垩纪)序列中的全球碳同位素事件。”日本学院论文集 B. 卷 79。
- DOI:
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- 影响因子:0
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Hasegawa, T.: "Possible application of carbon isotope stratigraphy for East Asian clastic sediments : a tool for stratigraphy or paleoenvironments"Memoir of the Fukui Prefectual Dinosaur Museum. (in press).
长谷川,T.:“碳同位素地层学在东亚碎屑沉积物中的可能应用:地层学或古环境的工具”福井县恐龙博物馆回忆录。
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- 影响因子:0
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Hasegawa, T.: "Cretaceous terrestrial paleoenvironments of northeastern Asia suggested from carbor isotope stratigraphy : increased atmospheric pCO_2-induced climate."Journal of Asian Earth Sciences. 21. 847-857 (2003)
Hasekawa, T.:“碳同位素地层学表明东北亚的白垩纪陆地古环境:大气 pCO_2 引起的气候增加。”亚洲地球科学杂志。
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- 影响因子:0
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HASEGAWA Takashi其他文献
HASEGAWA Takashi的其他文献
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{{ truncateString('HASEGAWA Takashi', 18)}}的其他基金
New paleothermometry for mudstone: utilization of calcreous nodules
泥岩古测温新方法:钙质结核的利用
- 批准号:
24654168 - 财政年份:2012
- 资助金额:
$ 2.18万 - 项目类别:
Grant-in-Aid for Challenging Exploratory Research
Global seesaw oscillation of botom water redox condition through Cretaceous OAE2
白垩纪 OAE2 底层水氧化还原条件的全球跷跷板振荡
- 批准号:
24403012 - 财政年份:2012
- 资助金额:
$ 2.18万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Warming pulse triggered by CO2 released during LIP formation: evaluating 20 kyr event during Cretaceous OAE2
LIP 形成过程中释放的 CO2 触发的变暖脉冲:评估白垩纪 OAE2 期间的 20 kyr 事件
- 批准号:
23340158 - 财政年份:2011
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$ 2.18万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Study on spin arrangement in two dimensional ferromagnetic-antiferromagnetic nanostructure
二维铁磁-反铁磁纳米结构自旋排列研究
- 批准号:
22760224 - 财政年份:2010
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$ 2.18万 - 项目类别:
Grant-in-Aid for Young Scientists (B)
Did change of deep water source amplify or diminish the climate fluctuation?: oceanic event stratigraphy of sulfur isotopes
深水源的变化是放大还是减弱了气候波动?:硫同位素的海洋事件地层学
- 批准号:
20340144 - 财政年份:2008
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$ 2.18万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Remarkable negative feedback against Cretaceous Oceanic Anoxic Event : evidence from Southwestern Pacific region
白垩纪海洋缺氧事件的显着负反馈:来自西南太平洋地区的证据
- 批准号:
20403016 - 财政年份:2008
- 资助金额:
$ 2.18万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Biochemical and Genetic Analysis of Perimenstrual Asthma Based on Epidermological Survey of Asthma in Niigata
基于新泻县哮喘流行病学调查的围经期哮喘生化及遗传学分析
- 批准号:
19591160 - 财政年份:2007
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$ 2.18万 - 项目类别:
Grant-in-Aid for Scientific Research (C)
Analysis of paleoclimate during OAE2. with world-highest resolution
OAE2 期间的古气候分析。
- 批准号:
18340164 - 财政年份:2006
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$ 2.18万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Analysis of Farmland by Visualizaiton Technique
农田可视化技术分析
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10306015 - 财政年份:1998
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$ 2.18万 - 项目类别:
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DEVELOPMENT OF EVALUATION METHOD FOR THE MATHEMATICS TEACHING BY TEAM TEACHING
数学小组教学评价方法的开发
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09680280 - 财政年份:1997
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$ 2.18万 - 项目类别:
Grant-in-Aid for Scientific Research (C)
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