globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:5859194
论文题名:
早古近纪陆相断陷型湖泊物质分异作用及其对PETM事件的响应:以济阳坳陷孔店组为例
其他题名: Material Differentiation and Its Response to thePETMEvents in Continental Fault Lake during the Early Paleogene Period:A Case Study of Kongdian Formation in Jiyang Depression
作者: 谭先锋1; 王佳2; 雷丽丹3; 况昊2; 高红灿2; 王伟庆4
刊名: 地球科学
ISSN: 1000-2383
出版年: 2016
卷: 41, 期:11, 页码:1893-1908
语种: 中文
中文关键词: PETM事件 ; 环境波动 ; 陆相断陷湖泊 ; 古近纪早期 ; 济阳坳陷 ; 石油地质
英文关键词: PETMevents ; environmental fluctuations ; continental fault Lake ; Early Paleogene period ; Jiyang depression ; petroleum geology
WOS学科分类: MINERALOGY
WOS研究方向: Mineralogy
中文摘要: 古近纪早期,地球上发生了古新世-始新世极热气候(PETM)事件,严重影响全球碳循环过程和海陆生态环境系统.依据普通薄片、元素分析、碳同位素、TOC等实验结果.研究了渤海湾盆地济阳断陷湖盆古新世-始新世时期的湖泊环境时空波动变化及其对PETM事件的响应,发现济阳断陷湖盆早期经历了多旋回的演化过程,湖盆中碎屑物质和化学物质的分异作用同时发生,陆地风化作用和化学沉积物质分异指示了极热气候的变化过程;该时期湖水为逐渐咸化的盐湖环境,具有空间的分带性和时间的阶段演化性,湖水咸化是热气候事件发生的直接响应;湖泊的时空波动演化经历了古新世-始新世时期的极热气候(PETM)事件,该事件早期湖泊尚未完全咸化,浮游生物比较繁盛,早期浮游植物对12 CO_2的吸收,会导致短暂的湖泊古生产力较高,但是随着湖盆逐渐咸化,生物的活动存活较难,主要以旱生植物为主,古生产力降到最低.由于过量的12 C吸收沉淀,造成湖泊沉积记录中的delta~(13) C明显负偏,最大可达5*10~(-3).由此证实全球PETM事件影响了古新世-始新世之交济阳断陷湖盆的时空演化和物质分异过程.
英文摘要: Paleocene Eocene climate(PETM)events in Early Paleogene period on the Earth had serious impact on the global carbon cycle process and the terrestrial and marine ecological environment system.In this paper,on the basis of general thinsections, elemental analysis,carbon isotope,TOC et al.,the impact of Paleocene Eocene lake environment of Jiyang rifted basin, Bohai bay on the temporal and spatial variation and response ofPETMis studied,and it is found Jiyang basin experienced early multicycle evolution processes,detrital material and chemical differentiation occurred at the same time in lacustrine basin,and terrestrial weathering and chemical sedimentary differentiation indicates the change of extreme climate.In this perod,the lake water experienced gradual salinization characterized by the spatial zoning and time-evolution stage,which is a direct response to the occurrence of hot climate events.Time-space evolution of the lake was subject toPETMevents.The lake was not fully salty in the early events with prosperous plankton.Early phytoplankton absorption of 12 CO_2 led to the higher productivity in the ancient Lake,which dropped to a minimum with the lake turning increasingly salty and more difficult for the survival. delta~(13) C of lacustrine sedimentary records are in obvious negative bias due to excessive 12 C absorption and precipitation,resulting in,a maximum of 5.It is confirmed that globalPETMevents affected the time-space evolution and differentiation process of material in Jiyang depression during Paleocene-Eocene.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/157075
Appears in Collections:气候变化事实与影响

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作者单位: 1.(武汉)中国地质大学, 复杂油气田勘探开发重庆市重点实验室
2.生物地质与环境地质国家重点实验室, 武汉, 湖北 430074, 中国
3.重庆科技学院石油与天然气工程学院, 复杂油气田勘探开发重庆市重点实验室, 重庆 401331, 中国
4.(武汉)中国地质大学, 生物地质与环境地质国家重点实验室, 武汉, 湖北 430074, 中国
5.中国石化胜利油田分公司地质科学研究院, 东营, 山东 257015, 中国

Recommended Citation:
谭先锋,王佳,雷丽丹,等. 早古近纪陆相断陷型湖泊物质分异作用及其对PETM事件的响应:以济阳坳陷孔店组为例[J]. 地球科学,2016-01-01,41(11):1893-1908
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