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      A Late Cretaceous amber biota from central Myanmar

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          Abstract

          Insect faunas are extremely rare near the latest Cretaceous with a 24-million-year gap spanning from the early Campanian to the early Eocene. Here, we report a unique amber biota from the Upper Cretaceous (uppermost Campanian ~72.1 Ma) of Tilin, central Myanmar. The chemical composition of Tilin amber suggests a tree source among conifers, indicating that gymnosperms were still abundant in the latest Campanian equatorial forests. Eight orders and 12 families of insects have been found in Tilin amber so far, making it the latest known diverse insect assemblage in the Mesozoic. The presence of ants of the extant subfamilies Dolichoderinae and Ponerinae supports that tropical forests were the cradle for the diversification of crown-group ants, and suggests that the turnover from stem groups to crown groups had already begun at ~72.1 Ma. Tilin amber biota fills a critical insect faunal gap and provides a rare insight into the latest Campanian forest ecosystem.

          Abstract

          The amber deposits from Kachin, Myanmar have provided numerous insights into life in the Cretaceous ~99 million years ago. Here, Zheng and colleagues describe a new Late Cretaceous amber biota from Tilin, Myanmar, dating from ~72 million years ago and preserving a diverse insect assemblage.

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          THREE NATURAL ZIRCON STANDARDS FOR U-TH-PB, LU-HF, TRACE ELEMENT AND REE ANALYSES

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            The Chicxulub asteroid impact and mass extinction at the Cretaceous-Paleogene boundary.

            The Cretaceous-Paleogene boundary approximately 65.5 million years ago marks one of the three largest mass extinctions in the past 500 million years. The extinction event coincided with a large asteroid impact at Chicxulub, Mexico, and occurred within the time of Deccan flood basalt volcanism in India. Here, we synthesize records of the global stratigraphy across this boundary to assess the proposed causes of the mass extinction. Notably, a single ejecta-rich deposit compositionally linked to the Chicxulub impact is globally distributed at the Cretaceous-Paleogene boundary. The temporal match between the ejecta layer and the onset of the extinctions and the agreement of ecological patterns in the fossil record with modeled environmental perturbations (for example, darkness and cooling) lead us to conclude that the Chicxulub impact triggered the mass extinction.
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              Correction of common lead in U–Pb analyses that do not report 204Pb

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                Author and article information

                Contributors
                suchin@hku.hk
                bowang@nigpas.ac.cn
                Journal
                Nat Commun
                Nat Commun
                Nature Communications
                Nature Publishing Group UK (London )
                2041-1723
                9 August 2018
                9 August 2018
                2018
                : 9
                : 3170
                Affiliations
                [1 ]ISNI 0000000119573309, GRID grid.9227.e, State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, , Chinese Academy of Sciences, ; 39 East Beijing Road, 210008 Nanjing, China
                [2 ]ISNI 0000000121742757, GRID grid.194645.b, Department of Earth Sciences, , The University of Hong Kong, Hong Kong Special Administrative Region, ; Hong Kong, China
                [3 ]ISNI 0000 0001 1482 4447, GRID grid.462934.e, University of Rennes, CNRS, , Géosciences Rennes - UMR 6118, ; 35000 Rennes, France
                [4 ]ISNI 0000 0001 2198 7527, GRID grid.417971.d, Department of Earth Sciences, , Indian Institute of Technology Bombay, ; Mumbai, 400076 India
                [5 ]ISNI 0000 0004 1936 7603, GRID grid.5337.2, School of Earth Sciences, , University of Bristol, ; Life Sciences Building, Tyndall Ave., Bristol, BS8 1TQ UK
                [6 ]ISNI 0000 0004 1799 3811, GRID grid.412508.a, Shandong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Minerals, , Shandong University of Science and Technology, ; 266590 Qingdao, Shandong China
                Author information
                http://orcid.org/0000-0003-0520-6780
                http://orcid.org/0000-0002-7973-0430
                http://orcid.org/0000-0002-4383-3956
                http://orcid.org/0000-0002-8001-9937
                Article
                5650
                10.1038/s41467-018-05650-2
                6085374
                30093646
                cc391b0d-4c42-4d90-97d1-4bbbd9f9f14b
                © The Author(s) 2018

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 19 January 2018
                : 20 July 2018
                Funding
                Funded by: FundRef https://doi.org/10.13039/501100001809, National Natural Science Foundation of China (National Science Foundation of China);
                Award ID: 41572010, 41622201, 41688103
                Award Recipient :
                Funded by: FundRef https://doi.org/10.13039/501100002367, Chinese Academy of Sciences (CAS);
                Award ID: XDPB05
                Award Recipient :
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