Strontium Isotope Evolution and Global Sea-level Changes of Carboniferous and Permian Marine Carbonate, Upper Yangtze Platform

HUANG Si jing; SHI He; ZHANG Meng; SHEN Li cheng; LIU Jie; WU Wen hui

The evoIution of strontium isotopic composition of originaI seawater is a function of geoIogicaI time, and mainIy controIIed by the gIobaI sea-IeveI changes. The evoIutionaI curves of the strontium isotopic composition of Carboniferous and Permian marine carbonate rocks, Upper Yangtze PIatform is guite consistent with trend of the sea-IeveI changes. This variation curve of the strontium isotope shows the foIIowing facts： 1）The gIobaI sea-IeveI rise is corresponding to the faIIing of strontium isotope. The point of the minimum vaIue of ⁸⁷ Sr /⁸⁶ Sr in the earIy Carboniferous is just the position of maximum fIooding surface for the period of earIy Carboniferous, of which the numeric age is 342 Ma. This key point is just Iocated at the boundary of Tournaisian and Visean, for the Huishui section in Guizhou of Province, which is Iocated at the boundary between Jiusi and Shangsi formation. 2）The Iate Carboniferous is a period of gIobaI sea-IeveI faIIing. 3）The Permian, from the beginning to the end, is a period of gIobaI sea-IeveI rise. During the Iate Permian, we can see that the sea IeveI was rising unceasingIy and the marine water became deepIy in short time. 4）The Iate Permian is provided with the strontium isotopic minimum of marine carbonate rocks throughout the Late PaIaeozoic, representing the gIobaI marine fIooding event. The numeric age of the fIooding is 250 Ma, which nears to the Permian-Triassic boundary. 5）The mass extinction at the boundary of Permian-Triassic is probabIy due to the gIobaI marine fIooding event of Iate Permian.

Strontium Isotope Evolution and Global Sea-level Changes of Carboniferous and Permian Marine Carbonate, Upper Yangtze Platform

State Key Laboratory of Oil/Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059

Received Date: 2000-12-26

Rev Recd Date: 2001-03-19

Publish Date: 2001-12-10

Key words:

Abstract: The evoIution of strontium isotopic composition of originaI seawater is a function of geoIogicaI time, and mainIy controIIed by the gIobaI sea-IeveI changes. The evoIutionaI curves of the strontium isotopic composition of Carboniferous and Permian marine carbonate rocks, Upper Yangtze PIatform is guite consistent with trend of the sea-IeveI changes. This variation curve of the strontium isotope shows the foIIowing facts： 1）The gIobaI sea-IeveI rise is corresponding to the faIIing of strontium isotope. The point of the minimum vaIue of ⁸⁷ Sr /⁸⁶ Sr in the earIy Carboniferous is just the position of maximum fIooding surface for the period of earIy Carboniferous, of which the numeric age is 342 Ma. This key point is just Iocated at the boundary of Tournaisian and Visean, for the Huishui section in Guizhou of Province, which is Iocated at the boundary between Jiusi and Shangsi formation. 2）The Iate Carboniferous is a period of gIobaI sea-IeveI faIIing. 3）The Permian, from the beginning to the end, is a period of gIobaI sea-IeveI rise. During the Iate Permian, we can see that the sea IeveI was rising unceasingIy and the marine water became deepIy in short time. 4）The Iate Permian is provided with the strontium isotopic minimum of marine carbonate rocks throughout the Late PaIaeozoic, representing the gIobaI marine fIooding event. The numeric age of the fIooding is 250 Ma, which nears to the Permian-Triassic boundary. 5）The mass extinction at the boundary of Permian-Triassic is probabIy due to the gIobaI marine fIooding event of Iate Permian.

HTML

Reference (1)

[1]

1.Palmer M R;Edmond J M The strontium isotope budget of the modern o cean 1989

2.Palmer M R;Elderfield H Sr isotope composition of sea water over t he past 75 Myr 1985

3.Denison R E;Koelpnick R B;Burke W H;Hetherington E A,Fletcher A Compositi on of the Mississippian Pennsylvanian and Permian seawater ⁸⁷ Sr/⁸⁶ Sr curve 1994

4.Raymo M E;Ruddiman W F;Froelich P N Influence of late Cenozoicmountain building on ocean geochemical cycles 1988

5.Capo R C;DePaolo D J Seawater strontium isotopic variations from 2.5 million years ago to the present 1990

6.Edmond J M Himalayan tectonics weathering processes and the stron tium isotope record in marine limestones 1992

7.Raymo M E;Ruddiman W F Tectonic forcing of late Cenozoic climate 1992

8.Hairuo Q;Barnes C R;BuhlD;Veizer J The strontium isotopic composition of Ordovician and Silurian brachiopods and conodonts:Relationships to geological events and implicationsfor coeval seawater[外文期刊] 1998(10)

9.Stoll H M;Schrag D P Effects of quaternary sea level cycles on stro ntium in seawater[外文期刊]1998(07)

10.Azmy K;Veizer J;Wenzel B;Bassett M G Copper P Silurian strontium isotope s tratigraphy 1999(04)

11.Zachos J C;Opdyke B N;Quinn T M;Jones C E,Halliday A N Early Ceno zoic glac iation antarctic weathering and seawater ⁸⁷ Sr/⁸⁶ Sr: Is the re a link[外文期刊] 2000(s1-3)

12.贵州省地层古生物工作队西南地区区域地层表:贵州省分册 1977

13.张正华;王治华;李昌全黔南二叠纪地层 1988

14.Palmer A R;Geissman J Geologic Time Scale 1999

15.陈洪德;覃建雄;田景春;彭军侯中建右江盆地层序充填动力学初探[期刊论文]-沉积学报 2000(02)

16.黄思静上扬子地台区晚古生代海相碳酸盐岩的碳、锶同位素研究 1997(01)

17.Vail p R;Mitchum R M;Thompson III S Seismic stratigraphy and glo bal chang es of sea level Part 4: Global cycles of relative changes of sea level 1977

18.殷鸿福二叠系-三叠系研究进展 1994(02)

19.殷鸿福;童金南;丁侮华;张克信赖旭龙杨子地区晚二叠世-中三叠世海平面变化 1994(05)

20.陈中强二叠纪末的全球淹没事件 1995(03)

21.McArthur J M Recent trends in strontium isotope stratigraphy[外文期刊] 1994

22.王增吉中国地层中国的石炭系 1990

Strontium Isotope Evolution and Global Sea-level Changes of Carboniferous and Permian Marine Carbonate, Upper Yangtze Platform

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related