Experimental Taphonomy of Artemia Reveals the Role of Endogenous
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Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
The Origin of Tetraradial Symmetry in Cnidarians
The origin of tetraradial symmetry in cnidarians JERZY DZIK, ANDRZEJ BALINSKI AND YUANLIN SUN Dzik, J., Balinski, A. & Sun, Y. 2017: The origin of tetraradial symmetry in cnidarians. Lethaia, DOI: 10.1111/let.12199. Serially arranged sets of eight septa-like structures occur in the basal part of phosphatic tubes of Sphenothallus from the early Ordovician (early Floian) Fenxi- ang Formation in Hubei Province of China. They are similar in shape, location and number, to cusps in chitinous tubes of extant coronate scyphozoan polyps, which supports the widely accepted cnidarian affinity of this problematic fossil. However, unlike the recent Medusozoa, the tubes of Sphenothallus are flattened at later stages of development, showing biradial symmetry. Moreover, the septa (cusps) in Sphenothallus are obliquely arranged, which introduces a bilateral component to the tube symmetry. This makes Sphenothallus similar to the Early Cambrian Paiutitubulites, having similar septa but with even more apparent bilat- eral disposition. Biradial symmetry also characterizes the Early Cambrian tubular fossil Hexaconularia, showing a similarity to the conulariids. However, instead of being strictly tetraradial like conulariids, Hexaconularia shows hexaradial symme- try superimposed on the biradial one. A conulariid with a smooth test showing signs of the ‘origami’ plicated closure of the aperture found in the Fenxiang For- mation supports the idea that tetraradial symmetry of conulariids resulted from geometrical constrains connected with this kind of closure. Its minute basal attachment surface makes it likely that the holdfasts characterizing Sphenothallus and advanced conulariids are secondary features. This concurs with the lack of any such holdfast in the earliest Cambrian Torellella, as well as in the possibly related Olivooides and Quadrapyrgites. -
The Early Cambrian Fossil Embryo Pseudooides Is a Direct-Developing Cnidarian, Not an Early Ecdysozoan
Downloaded from http://rspb.royalsocietypublishing.org/ on December 13, 2017 The early Cambrian fossil embryo rspb.royalsocietypublishing.org Pseudooides is a direct-developing cnidarian, not an early ecdysozoan Baichuan Duan1,2, Xi-Ping Dong2, Luis Porras3, Kelly Vargas3, Research John A. Cunningham3 and Philip C. J. Donoghue3 Cite this article: Duan B, Dong X-P, Porras L, 1Research Center for Islands and Coastal Zone, First Institute of Oceanography, State Oceanic Administration, Vargas K, Cunningham JA, Donoghue PCJ. Qingdao 266061, People’s Republic of China 2017 The early Cambrian fossil embryo 2School of Earth and Space Science, Peking University, Beijing 100871, People’s Republic of China 3School of Earth Sciences, University of Bristol, Life Sciences Building, Tyndall Avenue, Bristol BS8 1TQ, UK Pseudooides is a direct-developing cnidarian, not an early ecdysozoan. Proc. R. Soc. B 284: BD, 0000-0003-2188-598X; X-PD, 0000-0001-5917-7159; LP, 0000-0002-2296-5706; KV, 0000-0003-1320-4195; JAC, 0000-0002-2870-1832; PCJD, 0000-0003-3116-7463 20172188. http://dx.doi.org/10.1098/rspb.2017.2188 Early Cambrian Pseudooides prima has been described from embryonic and post-embryonic stages of development, exhibiting long germ-band develop- ment. There has been some debate about the pattern of segmentation, but this interpretation, as among the earliest records of ecdysozoans, has been Received: 29 September 2017 generally accepted. Here, we show that the ‘germ band’ of P. prima embryos Accepted: 14 November 2017 separates along its mid axis during development, with the transverse furrows between the ‘somites’ unfolding into the polar aperture of the ten- sided theca of Hexaconularia sichuanensis, conventionally interpreted as a scyphozoan cnidarian; co-occurring post-embryonic remains of ecdysozoans are unrelated. -
The Palaeontology Newsletter
The Palaeontology Newsletter Contents 90 Editorial 2 Association Business 3 Association Meetings 11 News 14 From our correspondents Legends of Rock: Marie Stopes 22 Behind the scenes at the Museum 25 Kinds of Blue 29 R: Statistical tests Part 3 36 Rock Fossils 45 Adopt-A-Fossil 48 Ethics in Palaeontology 52 FossilBlitz 54 The Iguanodon Restaurant 56 Future meetings of other bodies 59 Meeting Reports 64 Obituary: David M. Raup 79 Grant and Bursary Reports 81 Book Reviews 103 Careering off course! 111 Palaeontology vol 58 parts 5 & 6 113–115 Papers in Palaeontology vol 1 parts 3 & 4 116 Virtual Palaeontology issues 4 & 5 117–118 Annual Meeting supplement >120 Reminder: The deadline for copy for Issue no. 91 is 8th February 2016. On the Web: <http://www.palass.org/> ISSN: 0954-9900 Newsletter 90 2 Editorial I watched the press conference for the publication on the new hominin, Homo naledi, with rising incredulity. The pomp and ceremony! The emotion! I wondered why all of these people were so invested just because it was a new fossil species of something related to us in the very recent past. What about all of the other new fossil species that are discovered every day? I can’t imagine an international media frenzy, led by deans and vice chancellors amidst a backdrop of flags and flashbulbs, over a new species of ammonite. Most other fossil discoveries and publications of taxonomy are not met with such fanfare. The Annual Meeting is a time for sharing these discoveries, many of which will not bring the scientists involved international fame, but will advance our science and push the boundaries of our knowledge and understanding. -
Evolution, Origins and Diversification of Parasitic Cnidarians
1 Evolution, Origins and Diversification of Parasitic Cnidarians Beth Okamura*, Department of Life Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom. Email: [email protected] Alexander Gruhl, Department of Symbiosis, Max Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359 Bremen, Germany *Corresponding author 12th August 2020 Keywords Myxozoa, Polypodium, adaptations to parasitism, life‐cycle evolution, cnidarian origins, fossil record, host acquisition, molecular clock analysis, co‐phylogenetic analysis, unknown diversity Abstract Parasitism has evolved in cnidarians on multiple occasions but only one clade – the Myxozoa – has undergone substantial radiation. We briefly review minor parasitic clades that exploit pelagic hosts and then focus on the comparative biology and evolution of the highly speciose Myxozoa and its monotypic sister taxon, Polypodium hydriforme, which collectively form the Endocnidozoa. Cnidarian features that may have facilitated the evolution of endoparasitism are highlighted before considering endocnidozoan origins, life cycle evolution and potential early hosts. We review the fossil evidence and evaluate existing inferences based on molecular clock and co‐phylogenetic analyses. Finally, we consider patterns of adaptation and diversification and stress how poor sampling might preclude adequate understanding of endocnidozoan diversity. 2 1 Introduction Cnidarians are generally regarded as a phylum of predatory free‐living animals that occur as benthic polyps and pelagic medusa in the world’s oceans. They include some of the most iconic residents of marine environments, such as corals, sea anemones and jellyfish. Cnidarians are characterised by relatively simple body‐plans, formed entirely from two tissue layers (the ectoderm and endoderm), and by their stinging cells or nematocytes. -
Life Cycle Evolution: Was the Eumetazoan Ancestor a Holopelagic, Planktotrophic Gastraea? Claus Nielsen
Life cycle evolution was the eumetazoan ancestor a holoplanktonic, planktotrophic gastraea? Nielsen, Claus Published in: BMC Evolutionary Biology DOI: 10.1186/1471-2148-13-171 Publication date: 2013 Document version Publisher's PDF, also known as Version of record Document license: CC BY Citation for published version (APA): Nielsen, C. (2013). Life cycle evolution: was the eumetazoan ancestor a holoplanktonic, planktotrophic gastraea? BMC Evolutionary Biology, 13, [171]. https://doi.org/10.1186/1471-2148-13-171 Download date: 25. sep.. 2021 Nielsen BMC Evolutionary Biology 2013, 13:171 http://www.biomedcentral.com/1471-2148/13/171 REVIEW Open Access Life cycle evolution: was the eumetazoan ancestor a holopelagic, planktotrophic gastraea? Claus Nielsen Abstract Background: Two theories for the origin of animal life cycles with planktotrophic larvae are now discussed seriously: The terminal addition theory proposes a holopelagic, planktotrophic gastraea as the ancestor of the eumetazoans with addition of benthic adult stages and retention of the planktotrophic stages as larvae, i.e. the ancestral life cycles were indirect. The intercalation theory now proposes a benthic, deposit-feeding gastraea as the bilaterian ancestor with a direct development, and with planktotrophic larvae evolving independently in numerous lineages through specializations of juveniles. Results: Information from the fossil record, from mapping of developmental types onto known phylogenies, from occurrence of apical organs, and from genetics gives no direct information about the ancestral eumetazoan life cycle; however, there are plenty of examples of evolution from an indirect development to direct development, and no unequivocal example of evolution in the opposite direction. Analyses of scenarios for the two types of evolution are highly informative. -
New Palaeoscolecid Worms from the Furongian
[Palaeontology, Vol. 55, Part 3, 2012, pp. 613–622] NEW PALAEOSCOLECID WORMS FROM THE FURONGIAN (UPPER CAMBRIAN) OF HUNAN, SOUTH CHINA: IS MARKUELIA AN EMBRYONIC PALAEOSCOLECID? by BAICHUAN DUAN1, XI-PING DONG1* and PHILIP C. J. DONOGHUE2* 1School of Earth and Space Sciences, Peking University, Beijing 100871, China; e-mails: [email protected]; [email protected] 2School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, UK; e-mail: [email protected] *Corresponding authors. Typescript received 8 August 2011; accepted in revised form 26 October 2011 Abstract: Three-dimensional fragments of palaeoscolecid an embryonic palaeoscolecid. The comparative anatomy of cuticle have been recovered from the Furongian (upper Markuelia and the co-occurring palaeoscolecids shows a Cambrian) of Hunan, South China. Extraordinary preserva- number of distinctions, particularly in the structure of the tion of the fossils shows exquisite surface details indicating a tail; all similarities are scalidophoran or introvertan (cyclone- three-layered structure of the cuticle. One new genus and uralian) symplesiomorphies. The available evidence does not two new species Dispinoscolex decorus gen. et sp. nov. and support the interpretation of Markuelia as an embryonic pal- Schistoscolex hunanensis sp. nov. are described. The co-occur- aeoscolecid. rence of these palaeoscolecid remains with those of Marku- elia hunanensis allowed us to test the hypothesis that Key words: Palaeoscolecida, Priapulida, Scalidophora, In- Markuelia, known hitherto only from embryonic remains, is troverta, Cycloneuralia, Wangcun Lagersta¨tte. T he Wangcun Lagersta¨tte in the Furongian (upper Cam- annelids (Whittard 1953), Conway Morris (1993) sug- brian) Bitiao Formation of Wangcun, Yongshun County, gested that they were, in effect, stem-members of Scalido- western Hunan, has yielded a small but three-dimensional phora (the clade comprised of the phyla Kinorhyncha, soft-bodied fauna. -
Evidence from the Microanatomy of Cambrian Tetramerous Cubozoans
Divergent evolution of medusozoan symmetric patterns: Title Evidence from the microanatomy of Cambrian tetramerous cubozoans from South China Han, Jian; Kubota, Shin; Li, Guoxiang; Ou, Qiang; Wang, Xing; Yao, Xiaoyong; Shu, Degan; Li, Yong; Uesugi, Kentaro; Author(s) Hoshino, Masato; Sasaki, Osamu; Kano, Harumasa; Sato, Tomohiko; Komiya, Tsuyoshi Citation Gondwana Research (2016), 31: 150-163 Issue Date 2016-03 URL http://hdl.handle.net/2433/204554 © 2015. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/; The full- text file will be made open to the public on 1 March 2018 in Right accordance with publisher's 'Terms and Conditions for Self- Archiving'.; This is not the published version. Please cite only the published version.; この論文は出版社版でありません。 引用の際には出版社版をご確認ご利用ください。 Type Journal Article Textversion author Kyoto University ÔØ ÅÒÙ×Ö ÔØ Divergent evolution of medusozoan symmetric patterns: Evidence from the microanatomy of Cambrian tetramerous cubozoans from South China Jian Han, Shin Kubota, Guoxiang Li, Qiang Ou, Xing Wang, Xiaoyong Yao, Degan Shu, Yong Li, Kentaro Uesugi, Masato Hoshino, Osamu Sasaki, Harumasa Kano, Tomohiko Sato, Tsuyoshi Komiya PII: S1342-937X(15)00010-6 DOI: doi: 10.1016/j.gr.2015.01.003 Reference: GR 1383 To appear in: Gondwana Research Received date: 16 March 2014 Revised date: 31 December 2014 Accepted date: 3 January 2015 Please cite this article as: Han, Jian, Kubota, Shin, Li, Guoxiang, Ou, Qiang, Wang, Xing, Yao, Xiaoyong, Shu, Degan, Li, Yong, Uesugi, Kentaro, Hoshino, Masato, Sasaki, Osamu, Kano, Harumasa, Sato, Tomohiko, Komiya, Tsuyoshi, Divergent evo- lution of medusozoan symmetric patterns: Evidence from the microanatomy of Cam- brian tetramerous cubozoans from South China, Gondwana Research (2015), doi: 10.1016/j.gr.2015.01.003 This is a PDF file of an unedited manuscript that has been accepted for publication. -
Was the Eumetazoan Ancestor a Holopelagic, Planktotrophic Gastraea? Claus Nielsen
Nielsen BMC Evolutionary Biology 2013, 13:171 http://www.biomedcentral.com/1471-2148/13/171 REVIEW Open Access Life cycle evolution: was the eumetazoan ancestor a holopelagic, planktotrophic gastraea? Claus Nielsen Abstract Background: Two theories for the origin of animal life cycles with planktotrophic larvae are now discussed seriously: The terminal addition theory proposes a holopelagic, planktotrophic gastraea as the ancestor of the eumetazoans with addition of benthic adult stages and retention of the planktotrophic stages as larvae, i.e. the ancestral life cycles were indirect. The intercalation theory now proposes a benthic, deposit-feeding gastraea as the bilaterian ancestor with a direct development, and with planktotrophic larvae evolving independently in numerous lineages through specializations of juveniles. Results: Information from the fossil record, from mapping of developmental types onto known phylogenies, from occurrence of apical organs, and from genetics gives no direct information about the ancestral eumetazoan life cycle; however, there are plenty of examples of evolution from an indirect development to direct development, and no unequivocal example of evolution in the opposite direction. Analyses of scenarios for the two types of evolution are highly informative. The evolution of the indirect spiralian life cycle with a trochophora larva from a planktotrophic gastraea is explained by the trochophora theory as a continuous series of ancestors, where each evolutionary step had an adaptational advantage. The loss of ciliated larvae in the ecdysozoans is associated with the loss of outer ciliated epithelia. A scenario for the intercalation theory shows the origin of the planktotrophic larvae of the spiralians through a series of specializations of the general ciliation of the juvenile. -
Paleontology
PALEONTOLOGY SPECIMEN CABINETS N All steel construction N Powder paint finish N Durable door seal N No adhesives N Reinforced for easy stacking N Sturdy steel trays LANE SCIENCE EQUIPMENT CORP. 225 West 34th Street Tel: 212-563-0663 Suite 1412 Fax: 212-465-9440 New York, NY 10122-1496 www.lanescience.com Downloaded from https://www.cambridge.org/core. IP address: 170.106.202.58, on 02 Oct 2021 at 23:29:58, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/jpa.2017.149 Downloaded from https://www.cambridge.org/core. IP address: 170.106.202.58, on 02 Oct 2021 at 23:29:58, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/jpa.2017.149 Downloaded from https://www.cambridge.org/core. IP address: 170.106.202.58, on 02 Oct 2021 at 23:29:58, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/jpa.2017.149 Downloaded from https://www.cambridge.org/core. IP address: 170.106.202.58, on 02 Oct 2021 at 23:29:58, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/jpa.2017.149 OGic OGic L al L al O S O S T O T O N N C C O O I I E E E E T L T L Y Y A A P P OFFICERS AND EDITORS OF THE PALEONTOLOGICAL SOCIETY Grand Patrons ANDREW H. -
Title Early Cambrian Pentamerous Cubozoan Embryos from South
Early cambrian pentamerous cubozoan embryos from South Title china. Han, Jian; Kubota, Shin; Li, Guoxiang; Yao, Xiaoyong; Yang, Author(s) Xiaoguang; Shu, Degan; Li, Yong; Kinoshita, Shunichi; Sasaki, Osamu; Komiya, Tsuyoshi; Yan, Gang Citation PloS one (2013), 8(8) Issue Date 2013-08-12 URL http://hdl.handle.net/2433/178655 © 2013 Han et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, Right which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Type Journal Article Textversion publisher Kyoto University Early Cambrian Pentamerous Cubozoan Embryos from South China Jian Han1*, Shin Kubota2, Guoxiang Li3, Xiaoyong Yao4, Xiaoguang Yang1, Degan Shu1, Yong Li4, Shunichi Kinoshita5, Osamu Sasaki5, Tsuyoshi Komiya6, Gang Yan7 1 Early Life Institute and Department of Geology and State Key Laboratory of Continental Dynamics, Northwest University, Xi’an, P.R. China, 2 Seto Marine Biological Laboratory, Field Science Education and Research Center, Kyoto University, Shirahama, Nishimuro, Wakayama, Japan, 3 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, China, 4 School of Earth Science and Land Resources, Key Laboratory of Western China’s Mineral Resources and Geological Engineering, Ministry of Education, Chang’an University, Xi’an, P.R. China, 5 Tohoku University Museum, Tohoku University, Aramaki, Aoba-ku, Sendai, Japan, 6 Department of Earth Science and Astronomy, Graduated School of Arts and Science, Tokyo University, Meguro-ku, Tokyo, Japan, 7 Key Laboratory of Unconventional Oil and Gas, China National Petroleum Corporation (CNPC), Langfang, P. -
Old Medusozoan from the Kuanchuanpu
[Palaeontology, 2017, pp. 1–15] ANATOMY AND AFFINITIES OF A NEW 535-MILLION-YEAR-OLD MEDUSOZOAN FROM THE KUANCHUANPU FORMATION, SOUTH CHINA by XING WANG1,2 ,JIANHAN1,*, JEAN VANNIER2,QIANGOU3,4, XIAOGUANG YANG1,KENTAROUESUGI5, OSAMU SASAKI6 and TSUYOSHI KOMIYA7 1Early Life Institute & Department of Geology, State Key Laboratory of Continental Dynamics, Northwest University, 229 Taibai Road, Xi’an, 710069, China; [email protected] 2UMR 5276 du CNRS, Laboratoire de geologie de Lyon: Terre, Planetes, Environnement, Universite Lyon 1, B^atiment GEODE, 2, rue Rapha€el Dubois, Villeurbanne, 69622, France 3Early Life Evolution Laboratory, School of Earth Sciences & Resources, University of Geosciences, Beijing, 100083, China 4Department of Zoology, University of Kassel, Kassel, 34132, Germany 5Japan Synchrotron Radiation Research Institute (JASRI) 1-1-1 Kouto, Sayo-cho, Sayo-gun, Hyogo Japan 6Tohoku University Museum, Tohoku University, 6-3 Aoba, Aramaki, Aoba-ku, Sendai, Japan 7Department of Earth Science & Astronomy, Graduate School of Arts and Sciences, The University of Tokyo, Tokyo, 153-8902, Japan *Corresponding author Typescript received 10 April 2017; accepted in revised form 30 June 2017 Abstract: We describe here Sinaster petalon gen. et sp. pockets. Although Sinaster cannot be straightforwardly nov., a new embryonic form from the c. 535 million-year- assigned to any crown-group within Medusozoa, the pres- old Kuanchuanpu Formation of South China (Ningqiang, ence of marginal lappets and endodermal lamellae suggests Shaanxi Province). The excellent three-dimensional, phos- that it is closer to Cubozoa and Scyphozoa than to any other phatic preservation of these microfossils allowed us to use group of modern cnidarians. The tentative placement of x-ray microtomographic techniques to make accurate recon- Sinaster within the stem-group Cubozoa is justified by the structions of their internal structures and to compare their presence of a velarium supported by a frenulum.