High-precision U-Pb geochronology of the Jurassic Yanliao Biota from Jianchang (western Liaoning Province, China): Age constraints on the rise of feathered dinosaurs and eutherian mammals

被引:31
作者
Chu, Zhuyin [1 ]
He, Huaiyu [1 ]
Ramezani, Jahandar [2 ]
Bowring, Samuel A. [2 ]
Hu, Dongyu [3 ]
Zhang, Lijun [3 ]
Zheng, Shaolin [3 ]
Wang, Xiaolin [4 ]
Zhou, Zhonghe [4 ]
Deng, Chenglong [1 ]
Guo, Jinghui [1 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
[2] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA USA
[3] Shenyang Normal Univ, Inst Paleontol, Shenyang, Peoples R China
[4] Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing, Peoples R China
关键词
YIXIAN FORMATION; LANQI FORMATION; DAOHUGOU BIOTA; 40AR/39AR AGE; JEHOL BIOTA; THEROPOD; ORIGIN; MANIRAPTORAN; CALIBRATION; DIVERGENCE;
D O I
10.1002/2016GC006529
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Yanliao Biota of northeastern China comprises the oldest feathered dinosaurs, transitional pterosaurs, as well as the earliest eutherian mammals, multituberculate mammals, and new euharamiyidan species that are key elements of the Mesozoic biotic record. Recent discovery of the Yanliao Biota in the Daxishan section near the town of Linglongta, Jianchang County in western Liaoning Province have greatly enhanced our knowledge of the transition from dinosaurs to birds, primitive to derived pterosaurs, and the early evolution of mammals. Nevertheless, fundamental questions regarding the correlation of fossil-bearing strata, rates of dinosaur and mammalian evolution, and their relationship to environmental change in deep time remain unresolved due to the paucity of precise and accurate temporal constraints. These limitations underscore the importance of placing the rich fossil record of Jianchang within a high-resolution chronostratigraphic framework that has thus far been hampered by the relatively low precision of in situ radioisotopic dating techniques. Here we present high-precision U-Pb zircon geochronology by the chemical abrasion isotope dilution thermal ionization mass spectrometry (CA-ID-TIMS) from three interstratified ash beds previously dated by secondary-ion mass spectrometry (SIMS) technique. The results constrain the key fossil horizons of the Daxishan section to an interval spanning 160.89 to 160.25 Ma with 2 sigma analytical uncertainties that range from +/- 46 to +/- 69 kyr. These data place the Yanliao Biota from Jianchang in the Oxfordian Stage of the Late Jurassic, and mark the Daxishan section as the site of Earth's oldest precisely dated feathered dinosaurs and eutherian mammals.
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页码:3983 / 3992
页数:10
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