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      Dinosaur bonebed amber from an original swamp forest soil

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          Abstract

          Dinosaur bonebeds with amber content, yet scarce, offer a superior wealth and quality of data on ancient terrestrial ecosystems. However, the preserved palaeodiversity and/or taphonomic characteristics of these exceptional localities had hitherto limited their palaeobiological potential. Here, we describe the amber from the Lower Cretaceous dinosaur bonebed of Ariño (Teruel, Spain) using a multidisciplinary approach. Amber is found in both a root layer with amber strictly in situ and a litter layer mainly composed of aerial pieces unusually rich in bioinclusions, encompassing 11 insect orders, arachnids, and a few plant and vertebrate remains, including a feather. Additional palaeontological data—charophytes, palynomorphs, ostracods— are provided. Ariño arguably represents the most prolific and palaeobiologically diverse locality in which fossiliferous amber and a dinosaur bonebed have been found in association, and the only one known where the vast majority of the palaeontological assemblage suffered no or low-grade pre-burial transport. This has unlocked unprecedentedly complete and reliable palaeoecological data out of two complementary windows of preservation—the bonebed and the amber—from the same site.

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          History of Insects

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            Taphonomy of insects in carbonates and amber

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              Arthropods in amber from the Triassic Period.

              The occurrence of arthropods in amber exclusively from the Cretaceous and Cenozoic is widely regarded to be a result of the production and preservation of large amounts of tree resin beginning ca. 130 million years (Ma) ago. Abundant 230 million-year-old amber from the Late Triassic (Carnian) of northeastern Italy has previously yielded myriad microorganisms, but we report here that it also preserves arthropods some 100 Ma older than the earliest prior records in amber. The Triassic specimens are a nematoceran fly (Diptera) and two disparate species of mites, Triasacarus fedelei gen. et sp. nov., and Ampezzoa triassica gen. et sp. nov. These mites are the oldest definitive fossils of a group, the Eriophyoidea, which includes the gall mites and comprises at least 3,500 Recent species, 97% of which feed on angiosperms and represents one of the most specialized lineages of phytophagous arthropods. Antiquity of the gall mites in much their extant form was unexpected, particularly with the Triassic species already having many of their present-day features (such as only two pairs of legs); further, it establishes conifer feeding as an ancestral trait. Feeding by the fossil mites may have contributed to the formation of the amber droplets, but we find that the abundance of amber during the Carnian (ca. 230 Ma) is globally anomalous for the pre-Cretaceous and may, alternatively, be related to paleoclimate. Further recovery of arthropods in Carnian-aged amber is promising and will have profound implications for understanding the evolution of terrestrial members of the most diverse phylum of organisms.
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                Author and article information

                Contributors
                Role: Reviewing Editor
                Role: Senior Editor
                Journal
                eLife
                Elife
                eLife
                eLife
                eLife Sciences Publications, Ltd
                2050-084X
                30 November 2021
                2021
                : 10
                : e72477
                Affiliations
                [1 ] Departament de Dinàmica de la Terra i de l’Oceà and Institut de Recerca de la Biodiversitat (IRBio), Facultat de Ciències de la Terra, Universitat de Barcelona, c/Martí i Franquès s/n, 08028 Barcelona Spain
                [2 ] Oxford University Museum of Natural History Oxford United Kingdom
                [3 ] Museo Geominero (IGME, CSIC), c/ Ríos Rosas 23 Madrid Spain
                [4 ] Fundación Conjunto Paleontológico de Teruel-Dinópolis/Museo Aragonés de Paleontología, Av. Sagunto s/n Teruel Spain
                [5 ] Université de Sfax, Faculté des Sciences de Sfax Sfax Tunisia
                [6 ] Université de Tunis El Manar II, Faculté des Sciences de Tunis, LR18 ES07 Tunis Tunisia
                [7 ] Department of Geology, University of Vienna, UZA 2 Vienna Austria
                [8 ] Departamento de Geodinámica, Estratigrafía y Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, Ciudad Universitaria Madrid Spain
                [9 ] Museo de Ciencias Naturales de Álava, c/ Siervas de Jesús 24, 01001 Vitoria-Gasteiz Spain
                [10 ] Institut de Ciència i Tecnologia Ambientals (ICTA), Edifici Z – ICTA-ICP, Universitat Autònoma de Barcelona Barcelona Spain
                [11 ] School of Chemistry and Biochemistry, Georgia Institute of Technology Atlanta United States
                [12 ] Departamento de Biología de Sistemas/Instituto de Investigación Química “Andrés del Río” (IQAR), Universidad de Alcalá, 28805, Alcalá de Henares Madrid Spain
                [13 ] Univ. Lyon, Université Claude Bernard Lyon 1, CNRS, ENTPE, UMR 5023 LEHNA Villeurbanne France
                [14 ] Departament de Botànica i Geologia, Facultat de Ciències Biològiques, Universitat de València, c/ Dr. Moliner 50 Burjassot Spain
                [15 ] Division of Invertebrate Zoology, American Museum of Natural History New York United States
                [16 ] Departamento de Biodiversidad, Ecología y Evolución, Facultad de Biología, Universidad Complutense de Madrid, c/ José Antonio Novais 12 Madrid Spain
                Chinese Academy of Sciences China
                Pennsylvania State University United States
                Chinese Academy of Sciences China
                Chinese Academy of Sciences China
                Chinese Academy of Sciences China
                Author information
                https://orcid.org/0000-0002-0232-1647
                https://orcid.org/0000-0002-2830-2639
                https://orcid.org/0000-0001-8312-6087
                https://orcid.org/0000-0003-4979-1117
                https://orcid.org/0000-0002-6369-6186
                https://orcid.org/0000-0002-1782-5346
                https://orcid.org/0000-0003-4349-738X
                https://orcid.org/0000-0003-0207-9819
                https://orcid.org/0000-0002-7164-9558
                https://orcid.org/0000-0003-4074-7400
                https://orcid.org/0000-0001-7201-9286
                https://orcid.org/0000-0003-2701-6558
                https://orcid.org/0000-0003-0367-4177
                https://orcid.org/0000-0002-4658-617X
                https://orcid.org/0000-0003-0911-2001
                https://orcid.org/0000-0002-4877-7754
                https://orcid.org/0000-0002-2233-5480
                Article
                72477
                10.7554/eLife.72477
                8631943
                34844669
                b89fd165-b608-4012-890f-6f6e8da140fb
                © 2021, Álvarez-Parra et al

                This article is distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use and redistribution provided that the original author and source are credited.

                History
                : 25 July 2021
                : 08 November 2021
                Funding
                Funded by: FundRef http://dx.doi.org/10.13039/100014440, Ministerio de Ciencia, Innovación y Universidades;
                Award ID: CGL2017-84419
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/100014440, Ministerio de Ciencia, Innovación y Universidades;
                Award ID: PGC2018-094034-B-C22
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100003329, Ministerio de Economía y Competitividad;
                Award ID: CGL2015-69805-P
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100002809, Generalitat de Catalunya;
                Award ID: 2017SGR-824
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100002809, Generalitat de Catalunya;
                Award ID: 2020FI_B1 00002
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100000769, Oxford University;
                Award ID: Museum Research Fellowship
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/100014440, Ministerio de Ciencia, Innovación y Universidades;
                Award ID: BES-2016-076469
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100001822, Austrian Academy of Sciences;
                Award ID: Project 661
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100007521, Université de Tunis;
                Award ID: LR18 ES07
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100003359, Generalitat Valenciana;
                Award ID: APOSTD2019
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100008530, European Regional Development Fund;
                Award ID: IGME13-4E-1518
                Award Recipient :
                The funders had no role in study design, data collection and interpretation, or the decision to submit the work for publication.
                Categories
                Research Article
                Evolutionary Biology
                Custom metadata
                The most prolific and oldest locality in which a rich dinosaur bonebed and fossiliferous amber have been found in association is revealed, allowing the reconstruction of an ancient terrestrial ecosystem with a detail and accuracy reached only exceptionally in palaeontology.

                Life sciences
                ecology,palaeobiology,resin production,autochthony,insects,cretaceous,none
                Life sciences
                ecology, palaeobiology, resin production, autochthony, insects, cretaceous, none

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