The Oldest Arthropod Body Fossils from the Cambrian Stage 1 (Fortunian) in South China

Total Page:16

File Type:pdf, Size:1020Kb

The Oldest Arthropod Body Fossils from the Cambrian Stage 1 (Fortunian) in South China BCG07-03 JpGU-AGU Joint Meeting 2020 The oldest arthropod body fossils from the Cambrian Stage 1 (Fortunian) in South China *KONO SENA1, Yukio Isozaki1, Tomohiko Sato2, Xingliang Zhang3, Wei Liu3 1. The University of Tokyo School of Arts &Sciences, 2. Department of Earth and Planetary Sciences, Tokyo Institute of Technology, 3. Northwest university, China The oldest arthropod body fossils hitherto known are trilobite (Abadiella) and bradoriid (Kunmingella) in the Chengjiang fauna from Lower Cambrian Stage 3 (ca. 517 Ma) in Yunnan, South China. In contrast, no arthropod fossil was reported in diversified small shelly fossils (SSFs) from the lowermost Cambrian (Fortunian and Stage2). Our latest litho- and bio-stratigraphical study on the lowermost Cambrian at the Hongjiachong section in the Chengjiang area identified for the first time 2 different types of bivalved arthropod body fossils. These 2 types with 2 specimens for each, occur from the Fortunian phosphorite (Zhongyicun Mb.), around the boundary horizon between the Anabarites trisulcatus-Protohertzina anabaricaSSF Assemblage Zone and Paragrobolilus subglobosus-Purella squamulosaAssemblage Zone. Type A: subtriangular, 0.4 mm long, anterior/posterior asymmetric, dorsal outline straight, outlines of ventral, posterior, and anterior margins slightly curved outward, carapace with reticulate ornamented, two segmented. Type B: 1.7 mm long, anterior/posterior asymmetric, oval shaped, carapace with smooth surface. The former type is similar to Cenozoic ostracods in general form and size, and in having reticulate ornamented two segments. The oldest ostracod was reported previously from the lowermost Ordovician (Tremadocian) in central England. On the other hand, the latter type is similar to bradoriid in general size and form, but without lobes. The oldest bradoriid was reported from the Cambrian Stage 3 in South China. The present new finding of the oldest (Fortunian) arthropod body fossils demonstrates that arthropod has appeared at least 18 Myr earlier than previously believed. Keywords: Cambrian, Fortunian, oldest, arthropod, SSF, Chengjiang ©2020. Japan Geoscience Union. All Right Reserved. - BCG07-03 -.
Recommended publications
  • Decoupled Evolution of Soft and Hard Substrate Communities During the Cambrian Explosion and Great Ordovician Biodiversification Event
    Decoupled evolution of soft and hard substrate communities during the Cambrian Explosion and Great Ordovician Biodiversification Event Luis A. Buatoisa,1, Maria G. Mánganoa, Ricardo A. Oleab, and Mark A. Wilsonc aDepartment of Geological Sciences, University of Saskatchewan, Saskatoon, SK, Canada S7N 5E2; bEastern Energy Resources Science Center, US Geological Survey, Reston, VA 20192; and cDepartment of Geology, The College of Wooster, Wooster, OH 44691 Edited by Steven M. Holland, University of Georgia, Athens, GA, and accepted by Editorial Board Member David Jablonski May 6, 2016 (received for review November 21, 2015) Contrasts between the Cambrian Explosion (CE) and the Great shed light on the natures of both radiations. Because there is still Ordovician Biodiversification Event (GOBE) have long been recog- controversy regarding Sepkoski’s nonstandardized curves of nized. Whereas the vast majority of body plans were established Phanerozoic taxonomic diversity (13–15), a rarefaction analysis as a result of the CE, taxonomic increases during the GOBE were was performed in an attempt to standardize diversity data. The manifested at lower taxonomic levels. Assessing changes of ichno- aims of this paper are to document the contrasting ichnodiversity diversity and ichnodisparity as a result of these two evolutionary and ichnodisparity trajectories in soft and hard substrate com- events may shed light on the dynamics of both radiations. The early munities during these two evolutionary events and to discuss the Cambrian (series 1 and 2) displayed a dramatic increase in ichnodi- possible underlying causes of this decoupled evolution. versity and ichnodisparity in softground communities. In contrast to this evolutionary explosion in bioturbation structures, only a few Results Cambrian bioerosion structures are known.
    [Show full text]
  • Appendix 3.Pdf
    A Geoconservation perspective on the trace fossil record associated with the end – Ordovician mass extinction and glaciation in the Welsh Basin Item Type Thesis or dissertation Authors Nicholls, Keith H. Citation Nicholls, K. (2019). A Geoconservation perspective on the trace fossil record associated with the end – Ordovician mass extinction and glaciation in the Welsh Basin. (Doctoral dissertation). University of Chester, United Kingdom. Publisher University of Chester Rights Attribution-NonCommercial-NoDerivatives 4.0 International Download date 26/09/2021 02:37:15 Item License http://creativecommons.org/licenses/by-nc-nd/4.0/ Link to Item http://hdl.handle.net/10034/622234 International Chronostratigraphic Chart v2013/01 Erathem / Era System / Period Quaternary Neogene C e n o z o i c Paleogene Cretaceous M e s o z o i c Jurassic M e s o z o i c Jurassic Triassic Permian Carboniferous P a l Devonian e o z o i c P a l Devonian e o z o i c Silurian Ordovician s a n u a F y r Cambrian a n o i t u l o v E s ' i k s w o Ichnogeneric Diversity k p e 0 10 20 30 40 50 60 70 S 1 3 5 7 9 11 13 15 17 19 21 n 23 r e 25 d 27 o 29 M 31 33 35 37 39 T 41 43 i 45 47 m 49 e 51 53 55 57 59 61 63 65 67 69 71 73 75 77 79 81 83 85 87 89 91 93 Number of Ichnogenera (Treatise Part W) Ichnogeneric Diversity 0 10 20 30 40 50 60 70 1 3 5 7 9 11 13 15 17 19 21 n 23 r e 25 d 27 o 29 M 31 33 35 37 39 T 41 43 i 45 47 m 49 e 51 53 55 57 59 61 c i o 63 z 65 o e 67 a l 69 a 71 P 73 75 77 79 81 83 n 85 a i r 87 b 89 m 91 a 93 C Number of Ichnogenera (Treatise Part W)
    [Show full text]
  • The Geologic Time Scale Is the Eon
    Exploring Geologic Time Poster Illustrated Teacher's Guide #35-1145 Paper #35-1146 Laminated Background Geologic Time Scale Basics The history of the Earth covers a vast expanse of time, so scientists divide it into smaller sections that are associ- ated with particular events that have occurred in the past.The approximate time range of each time span is shown on the poster.The largest time span of the geologic time scale is the eon. It is an indefinitely long period of time that contains at least two eras. Geologic time is divided into two eons.The more ancient eon is called the Precambrian, and the more recent is the Phanerozoic. Each eon is subdivided into smaller spans called eras.The Precambrian eon is divided from most ancient into the Hadean era, Archean era, and Proterozoic era. See Figure 1. Precambrian Eon Proterozoic Era 2500 - 550 million years ago Archaean Era 3800 - 2500 million years ago Hadean Era 4600 - 3800 million years ago Figure 1. Eras of the Precambrian Eon Single-celled and simple multicelled organisms first developed during the Precambrian eon. There are many fos- sils from this time because the sea-dwelling creatures were trapped in sediments and preserved. The Phanerozoic eon is subdivided into three eras – the Paleozoic era, Mesozoic era, and Cenozoic era. An era is often divided into several smaller time spans called periods. For example, the Paleozoic era is divided into the Cambrian, Ordovician, Silurian, Devonian, Carboniferous,and Permian periods. Paleozoic Era Permian Period 300 - 250 million years ago Carboniferous Period 350 - 300 million years ago Devonian Period 400 - 350 million years ago Silurian Period 450 - 400 million years ago Ordovician Period 500 - 450 million years ago Cambrian Period 550 - 500 million years ago Figure 2.
    [Show full text]
  • The Cambrian Explosion: a Big Bang in the Evolution of Animals
    The Cambrian Explosion A Big Bang in the Evolution of Animals Very suddenly, and at about the same horizon the world over, life showed up in the rocks with a bang. For most of Earth’s early history, there simply was no fossil record. Only recently have we come to discover otherwise: Life is virtually as old as the planet itself, and even the most ancient sedimentary rocks have yielded fossilized remains of primitive forms of life. NILES ELDREDGE, LIFE PULSE, EPISODES FROM THE STORY OF THE FOSSIL RECORD The Cambrian Explosion: A Big Bang in the Evolution of Animals Our home planet coalesced into a sphere about four-and-a-half-billion years ago, acquired water and carbon about four billion years ago, and less than a billion years later, according to microscopic fossils, organic cells began to show up in that inert matter. Single-celled life had begun. Single cells dominated life on the planet for billions of years before multicellular animals appeared. Fossils from 635,000 million years ago reveal fats that today are only produced by sponges. These biomarkers may be the earliest evidence of multi-cellular animals. Soon after we can see the shadowy impressions of more complex fans and jellies and things with no names that show that animal life was in an experimental phase (called the Ediacran period). Then suddenly, in the relatively short span of about twenty million years (given the usual pace of geologic time), life exploded in a radiation of abundance and diversity that contained the body plans of almost all the animals we know today.
    [Show full text]
  • Trace Fossils and Substrates of the Terminal Proterozoic–Cambrian Transition: Implications for the Record of Early Bilaterians and Sediment Mixing
    Trace fossils and substrates of the terminal Proterozoic–Cambrian transition: Implications for the record of early bilaterians and sediment mixing Mary L. Droser*†,So¨ ren Jensen*, and James G. Gehling‡ *Department of Earth Sciences, University of California, Riverside, CA 92521; and ‡South Australian Museum, Division of Natural Sciences, North Terrace, Adelaide 5000, South Australia, Australia Edited by James W. Valentine, University of California, Berkeley, CA, and approved August 16, 2002 (received for review May 29, 2002) The trace fossil record is important in determining the timing of the appearance of bilaterian animals. A conservative estimate puts this time at Ϸ555 million years ago. The preservational potential of traces made close to the sediment–water interface is crucial to detecting early benthic activity. Our studies on earliest Cambrian sediments suggest that shallow tiers were preserved to a greater extent than typical for most of the Phanerozoic, which can be attributed both directly and indirectly to the low levels of sediment mixing. The low levels of sediment mixing meant that thin event beds were preserved. The shallow depth of sediment mixing also meant that muddy sediments were firm close to the sediment–water interface, increasing the likelihood of recording shallow-tier trace fossils in muddy sed- iments. Overall, trace fossils can provide a sound record of the onset of bilaterian benthic activity. he appearance and subsequent diversification of bilaterian Tanimals is a topic of current controversy (refs. 1–7; Fig. 1). Three principal sources of evidence exist: body fossils, trace fossils (trails, tracks, and burrows of animal activity recorded in the sedimentary record), and divergence times calculated by means of a molecular ‘‘clock.’’ The body fossil record indicates a geologically rapid diversification of bilaterian animals not much earlier than the Precambrian–Cambrian boundary, the so-called Cambrian explosion.
    [Show full text]
  • A Fundamental Precambrian–Phanerozoic Shift in Earth's Glacial
    Tectonophysics 375 (2003) 353–385 www.elsevier.com/locate/tecto A fundamental Precambrian–Phanerozoic shift in earth’s glacial style? D.A.D. Evans* Department of Geology and Geophysics, Yale University, P.O. Box 208109, 210 Whitney Avenue, New Haven, CT 06520-8109, USA Received 24 May 2002; received in revised form 25 March 2003; accepted 5 June 2003 Abstract It has recently been found that Neoproterozoic glaciogenic sediments were deposited mainly at low paleolatitudes, in marked qualitative contrast to their Pleistocene counterparts. Several competing models vie for explanation of this unusual paleoclimatic record, most notably the high-obliquity hypothesis and varying degrees of the snowball Earth scenario. The present study quantitatively compiles the global distributions of Miocene–Pleistocene glaciogenic deposits and paleomagnetically derived paleolatitudes for Late Devonian–Permian, Ordovician–Silurian, Neoproterozoic, and Paleoproterozoic glaciogenic rocks. Whereas high depositional latitudes dominate all Phanerozoic ice ages, exclusively low paleolatitudes characterize both of the major Precambrian glacial epochs. Transition between these modes occurred within a 100-My interval, precisely coeval with the Neoproterozoic–Cambrian ‘‘explosion’’ of metazoan diversity. Glaciation is much more common since 750 Ma than in the preceding sedimentary record, an observation that cannot be ascribed merely to preservation. These patterns suggest an overall cooling of Earth’s longterm climate, superimposed by developing regulatory feedbacks
    [Show full text]
  • The Ediacaran–Cambrian Transition: the Emerging Record from Small Carbonaceous Fossils (Scfs)
    38 The Ediacaran–Cambrian transition: the emerging record from Small Carbonaceous Fossils (SCFs) Ben J. Slater1, Thomas H.P. Harvey2, Romain Guilbaud3, Sebastian Willman1, Graham E. Budd1, Nicholas J. Butterfield4. 1Department of Earth Sciences (Palaeobiology), Uppsala University, Villavägen 16, SE-75236 Uppsala, Sweden ([email protected]) 2School of Geography, Geology and the Environment, University of Leicester, Leicester LE1 7RH, UK 3Lancaster Environment Centre, Lancaster University, Lancaster, LA1 4YQ, UK. 4Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK Abstract.––The most profound change in the fossil record is centered on the Ediacaran–Cambrian transition. Sediments deposited near to this boundary record the first complex trace fossils, the first animal biomineralizers and the earliest fossils of the major animal groups that came to define the subsequent Phanerozoic fossil record. Here we discuss how the emerging record of small carbonaceous fossils (SCFs) is shedding new light on unmineralized aspects of the biota from this critical evolutionary transition. The new SCFs record complements currently established records from trace fossils and biomineralized shelly-remains in reconstructing the broader scale macroevolutionary patterns of this transition, but via an entirely different taphonomic window. SCFs extend the record of multiple major animal groups, improve our picture of protistan diversity from this interval, and reveal new data on elements of the biota that span the Ediacaran–Cambrian boundary. Key words: small carbonaceous fossils; bilateria; Burgess Shale-type preservation; Ediacaran; Terreneuvian. The dramatic changes in the fossil record across subsequent Cambrian radiation (Butterfield, the Ediacaran–Cambrian transition seemingly 2003; Slater et al., 2018a).
    [Show full text]
  • The Weeks Formation Konservat-Lagerstätte and the Evolutionary Transition of Cambrian Marine Life
    Downloaded from http://jgs.lyellcollection.org/ by guest on October 1, 2021 Review focus Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2018-042 The Weeks Formation Konservat-Lagerstätte and the evolutionary transition of Cambrian marine life Rudy Lerosey-Aubril1*, Robert R. Gaines2, Thomas A. Hegna3, Javier Ortega-Hernández4,5, Peter Van Roy6, Carlo Kier7 & Enrico Bonino7 1 Palaeoscience Research Centre, School of Environmental and Rural Science, University of New England, Armidale, NSW 2351, Australia 2 Geology Department, Pomona College, Claremont, CA 91711, USA 3 Department of Geology, Western Illinois University, 113 Tillman Hall, 1 University Circle, Macomb, IL 61455, USA 4 Department of Zoology, University of Cambridge, Downing Street, Cambridge CB2 3EJ, UK 5 Museum of Comparative Zoology and Department of Organismic and Evolutionary Biology, Harvard University, 26 Oxford Street, Cambridge, MA 02138, USA 6 Department of Geology, Ghent University, Krijgslaan 281/S8, B-9000 Ghent, Belgium 7 Back to the Past Museum, Carretera Cancún, Puerto Morelos, Quintana Roo 77580, Mexico R.L.-A., 0000-0003-2256-1872; R.R.G., 0000-0002-3713-5764; T.A.H., 0000-0001-9067-8787; J.O.-H., 0000-0002- 6801-7373 * Correspondence: [email protected] Abstract: The Weeks Formation in Utah is the youngest (c. 499 Ma) and least studied Cambrian Lagerstätte of the western USA. It preserves a diverse, exceptionally preserved fauna that inhabited a relatively deep water environment at the offshore margin of a carbonate platform, resembling the setting of the underlying Wheeler and Marjum formations. However, the Weeks fauna differs significantly in composition from the other remarkable biotas of the Cambrian Series 3 of Utah, suggesting a significant Guzhangian faunal restructuring.
    [Show full text]
  • Late Precambrian (Adaptive Radiation/Cambrian/Evolution/Paleontology/Predation)
    Proc. Nat. Acad. Sci. USA Vol. 70, No. 5, pp. 1486-1489, May 1973 An Ecological Theory for the Sudden Origin of Multicellular Life in the Late Precambrian (adaptive radiation/Cambrian/evolution/paleontology/predation) STEVEN M. STANLEY Department of Earth and Planetary Sciences, The Johns Hopkins University, Baltimore, Maryland 21218 Communicated by Hans P. Eugster, March 16, 1973 ABSTRACT According to modern ecological theory, Eukaryotic organisms arose earlier than 1300 million years high diversity at any trophic level of a community is pos- ago, and perhaps even earlier than 1700 million years ago, sible only under the influence of cropping. Until herbivores evolved, single-celled algae of the Precambrian were re- but were probably haploid and asexual at first. The oldest source-limited, and a small number of species saturated convincing evidence of sexuality comes from spore-like uni- aquatic environments. In the near-absence of vacant cells in the 900 million year-old Bitter Springs fossil flora. niches, life diversified slowly. Because the changes re- The advent of sexuality should have greatly increased genetic quired to produce the first algae-eating heterotrophs were therefore delayed, the entire system was self-limiting. variability and correspondingly increased rates of evolution- When the "heterotroph barrier" was finally crossed in the ary diversification. It is then puzzling that the Bitter Springs late Precambrian, herbivorous and carnivorous protists flora and various other fossil assemblages of similar age are arose almost simultaneously, for no major biological dif- impoverished relative to modern eukaryote assemblages. ferences separate the two groups. These events automati- They have yielded only simple spheroidal unicells, none of cally triggered the formation of a series of self-propagat- ing feedback systems of diversification between adjacent which exhibits features typical of even moderately advanced trophic levels.
    [Show full text]
  • Low-Latitude Origins of the Four Phanerozoic Evolutionary Faunas
    bioRxiv preprint doi: https://doi.org/10.1101/866186; this version posted December 6, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. Low-Latitude Origins of the Four Phanerozoic Evolutionary Faunas A. Rojas1*, J. Calatayud1, M. Kowalewski2, M. Neuman1, and M. Rosvall1 1Integrated Science Lab, Department of Physics, Umeå University, SE-901 87 Umeå, Sweden 5 2Florida Museum of Natural History, Division of Invertebrate Paleontology, University of Florida, Gainesville, FL 32611, USA *Correspondence to: [email protected] Abstract: Sepkoski’s hypothesis of Three Great Evolutionary Faunas that dominated 10 Phanerozoic oceans represents a foundational concept of macroevolutionary research. However, the hypothesis lacks spatial information and fails to recognize ecosystem changes in Mesozoic oceans. Using a multilayer network representation of fossil occurrences, we demonstrate that Phanerozoic oceans sequentially harbored four evolutionary faunas: Cambrian, Paleozoic, Mesozoic, and Cenozoic. These mega-assemblages all emerged at low latitudes and dispersed 15 out of the tropics. The Paleozoic–Mesozoic transition was abrupt, coincident with the Permian mass extinction, whereas the Mesozoic–Cenozoic transition was protracted, concurrent with gradual ecological shifts posited by the Mesozoic Marine Revolution. These findings support the notion that long-term ecological changes, historical contingencies, and major geological events all have played crucial roles in shaping the evolutionary history of marine animals. 20 One Sentence Summary: Network analysis reveals that Phanerozoic oceans harbored four evolutionary faunas with variable tempo and underlying causes.
    [Show full text]
  • Oxygen, Ecology, and the Cambrian Radiation of Animals
    Oxygen, Ecology, and the Cambrian Radiation of Animals The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Sperling, Erik A., Christina A. Frieder, Akkur V. Raman, Peter R. Girguis, Lisa A. Levin, and Andrew H. Knoll. 2013. Oxygen, Ecology, and the Cambrian Radiation of Animals. Proceedings of the National Academy of Sciences 110, no. 33: 13446–13451. Published Version doi:10.1073/pnas.1312778110 Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:12336338 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA Oxygen, ecology, and the Cambrian radiation of animals Erik A. Sperlinga,1, Christina A. Friederb, Akkur V. Ramanc, Peter R. Girguisd, Lisa A. Levinb, a,d, 2 Andrew H. Knoll Affiliations: a Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, 02138 b Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, 92093- 0218 c Marine Biological Laboratory, Department of Zoology, Andhra University, Waltair, Visakhapatnam – 530003 d Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, 02138 1 Correspondence to: [email protected] 2 Correspondence to: [email protected] PHYSICAL SCIENCES: Earth, Atmospheric and Planetary Sciences BIOLOGICAL SCIENCES: Evolution Abstract: 154 words Main Text: 2,746 words Number of Figures: 2 Number of Tables: 1 Running Title: Oxygen, ecology, and the Cambrian radiation Keywords: oxygen, ecology, predation, Cambrian radiation The Proterozoic-Cambrian transition records the appearance of essentially all animal body plans (phyla), yet to date no single hypothesis adequately explains both the timing of the event and the evident increase in diversity and disparity.
    [Show full text]
  • Cambrian Transition in the Southern Great Basin
    The Sedimentary Record 2000; Shen and Schidlowski, 2000). Due to The Precambrian- endemic biotas and facies control, it is diffi- cult to correlate directly between siliciclas- Cambrian Transition in the tic- and carbonate-dominated successions. This is particularly true for the PC-C boundary interval because lowermost Southern Great Basin, USA Cambrian biotas are highly endemic and Frank A. Corsetti James W.Hagadorn individual, globally distributed guide fossils Department of Earth Science Department of Geology are lacking (Landing, 1988; Geyer and University of Southern California Amherst College Shergold, 2000). Los Angeles, CA 90089-0740 Amherst, MA 01002 Determination of a stratigraphic bound- [email protected] [email protected] ary generates a large amount of interest because it provides scientists with an oppor- ABSTRACT:The Precambrian-Cambrian boundary presents an interesting tunity to address a variety of related issues, stratigraphic conundrum: the trace fossil used to mark and correlate the base of the including whether the proposed boundary Cambrian, Treptichnus pedum, is restricted to siliciclastic facies, whereas position marks a major event in Earth histo- biomineralized fossils and chemostratigraphic signals are most commonly obtained ry. Sometimes the larger-scale meaning of from carbonate-dominated sections.Thus, it is difficult to correlate directly between the particular boundary can be lost during many of the Precambrian-Cambrian boundary sections, and to assess details of the the process of characterization. This is timing of evolutionary events that transpired during this interval of time.Thick demonstrated in a plot of PC-C boundary sections in the White-Inyo region of eastern California and western Nevada, USA, papers through time (Fig.
    [Show full text]