[Submitted to the Journal Papers in Palaeontology in July 29, 2019]

Total Page:16

File Type:pdf, Size:1020Kb

[Submitted to the Journal Papers in Palaeontology in July 29, 2019] bioRxiv preprint doi: https://doi.org/10.1101/719153; this version posted October 9, 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 The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity.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. 1 [Submitted to the journal Papers in Palaeontology in july 29, 2019] 2 3 SYSTEMATIC REVISION AND REDEFINITION OF THE GENUS SCIRROTHERIUM 4 EDMUND & THEODOR, 1997 (CINGULATA, PAMPATHERIIDAE): IMPLICATIONS 5 FOR THE ORIGIN OF PAMPATHERIIDS AND THE EVOLUTION OF THE SOUTH 6 AMERICAN LINEAGE INCLUDING HOLMESINA 7 8 By KEVIN JIMÉNEZ-LARA1,2 9 1 División de Paleontología de Vertebrados, Museo de La Plata, Facultad de Ciencias 10 Naturales y Museo, Universidad Nacional de La Plata, Paseo del Bosque s/n, B1900FWA 11 La Plata, Argentina. 12 2CONICET, Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina. 13 e-mail: [email protected] 14 15 Abstract: The intrageneric relationships of the pampatheriid genus Scirrotherium and its 16 affinities with supposedly related genera, i.e. Kraglievichia and Holmesina, are revised 17 through parsimony phylogenetic analyses and new comparative morphological 18 descriptions. For this work was analyzed unpublished material of pampatheriids (numerous 19 osteoderms, one partial skull and a few postcranial bones) from Neogene formations of 20 Colombia. The results show that Scirrotherium is paraphyletic if we include all its referred 21 species, i.e. Scirrotherium hondaensis, S. carinatum and S. antelucanus. The species S. bioRxiv preprint doi: https://doi.org/10.1101/719153; this version posted October 9, 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 The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity.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. 22 carinatum is closer to Kraglievichia paranensis than to S. hondaensis or S. antelucanus, 23 then it is proposed the new name K. carinatum comb. nov. The relationships between S. 24 hondaensis and S. antelucanus could not be resolved, so these species should be designated 25 in aphyly. In spite of failing to recover S. hondaensis and S. antelucanus as one single 26 clade, here is preferred to maintain the generic name Scirrotherium in both species from 27 diagnostic evidence. New emended diagnoses for Scirrotherium, S. hondaensis and 28 Kraglievichia are provided. The genus Holmesina was found monophyletic and located as 29 the sister clade of Scirrotherium + Kraglievichia. The evolutionary and biogeographical 30 implications of the new phylogeny and taxonomical re-arrangements are discussed. It is 31 claimed a possible geographical origin of the family Pampatheriidae and Scirrotherium in 32 low latitudes of South America as early as Early Miocene (Burdigalian) times. The South 33 American ancestor or sister taxon of Holmesina is predicted as morphologically more 34 similar to Scirrotherium than to Kraglievichia. 35 Key words: Pampatheriidae, Scirrotherium, Kraglievichia, Holmesina, Great American 36 Biotic Interchange, Neogene. 37 38 The pampatheriids (Pampatheriidae) are a morphologically conservative extinct clade of 39 glyptodontoid cingulates or highly armored xenartrans (Glyptodontoidea sensu McKenna & 40 Bell 1997) with medium-to-large body sizes (Edmund 1985; Góis et al. 2013). They were 41 distributed from the Neogene to the Early Holocene in numerous localities of South 42 America (their native range), Central America, Mexico and the United States (Edmund 43 1985; Vizcaíno et al. 1998; Rincón et al. 2014; Góis et al. 2015 and references there). As 44 the modern armadillos (Dasypodidae), pampatheriids have a flexible carapace by the bioRxiv preprint doi: https://doi.org/10.1101/719153; this version posted October 9, 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. 45 presence of three transverse bands of imbricated osteoderms which conform a kind of 46 “articulation” between the scapular and pelvic shields (Edmund 1985). The pampatheriids 47 also have multiple features, especially in their skull and mandible, which, collectively, 48 define them as the sister group of glyptodontids –Glyptodontidae (Gaudin 2004; Gaudin & 49 Wible 2006; Billet et al. 2011; Delsuc et al. 2012), namely deep horizontal mandibular 50 ramus, laterally-directed zygomatic root, transversely-wide glenoid fossa, rough pterygoids, 51 among others (Gaudin & Wible, 2006). 52 The fossil record of Pampatheriidae is mainly represented by isolated specimens, of which 53 most of them are osteoderms and, in lesser extent, skulls, mandibles and postcranial bones; 54 fairly complete and articulated skeletons are uncommon (Edmund 1985; Góis 2013). Due 55 the above, the systematics of this xenartran group has historically been based on 56 osteodermal characters (Edmund 1985, 1987; Góis et al. 2013), as has been the case with 57 other cingulate clades. Overall, nearly two tens of pampatheriid species and seven genera 58 are known (Góis 2013). The latter conform two possible subfamilial lineages: (1) that 59 including to the genera Plaina and Pampatherium; and (2) that comprising the genera 60 Scirrotherium, Kraglievichia and Holmesina (Edmund 1985). However, it does not exist in 61 the scientific literature a published phylogenetic analysis on the relationships between the 62 different pampatheriid genera. Only Góis (2013) performed a phylogenetic analysis for 63 these taxa, but his results have not been published. In Góis’s consensus tree, it was 64 corroborated the hypothesis by Edmund (1985) on the two subfamilial lineages. 65 The genus Scirrotherium is the oldest known pampatheriid in the fossil record (Góis et al. 66 2013; Rincón et al. 2014) and one of the four Miocene genera (the other ones are 67 Kraglievichia Castellanos 1927; Vassallia Castellanos, 1927; and Plaina Castellanos, bioRxiv preprint doi: https://doi.org/10.1101/719153; this version posted October 9, 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. 68 1937). This taxon was originally described by Edmund & Theodor (1997) from 69 craniomandibular, postcranial and osteodermal specimens collected in the Middle Miocene 70 (Serravalian) sedimentary sequence of the La Venta area, southwestern Colombia. These 71 authors interpreted that the only known species in that time and type species, Scirrotherium 72 hondaensis, has plesiomorphic traits in its osteological morphology which are expected for 73 its antiquity. Additionally, they highlighted morphological similarity of S. hondaensis with 74 the species Vassallia minuta (Late Miocene of southern and central South America; De 75 Iullis & Edmund 2002), more than with any other pampatheriid. 76 Later, Góis et al. (2013) described a second species for Scirrotherium, S. carinatum, from 77 the Late Miocene (Tortonian) of northeastern and southern of Argentina-northwestern 78 Brazil. In northeastern Argentina (Entre Ríos Province), S. carinatum shares basal 79 stratigraphic levels (“Conglomerado Osífero”, literally ‘bone-bearing conglomerate’) in the 80 Ituzaingó Formation with the middle-sized pampatheriid Kraglievichia paranensis (Góis et 81 al. 2013; Scillato-Yané et al. 2013), a taxon different but not distantly related to 82 Scirrotherium as previously indicated. The species S. carinatum, based exclusively on 83 osteoderms of different regions of the armored carapace, has a body size comparable or 84 slightly smaller than that of S. hondaensis (Góis et al. 2013). 85 The phylogenetic analysis conducted by Góis (2013) recovered in polytomy to S. carinatum 86 and S. hondaensis, being one of these species or both of them the sister taxon/taxa of the 87 clade Kraglievichia + Holmesina (except H. floridanus). It is notorious the non-basal 88 position of the Scirrotherium species within the general topology of the cladogram despite 89 they conform the oldest known genus. Instead, these species are closely placed to widely 90 recognized terminal taxa, i.e. Holmesina spp. (Edmund 1985, 1987; Gaudin & Lyon 2017). bioRxiv preprint doi: https://doi.org/10.1101/719153; this version posted October 9, 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. 91 If this result is correct, it would indicate a significantly long ghost lineage at the base of the 92 evolutionary tree of Pampatheriidae. 93 Góis found phylogenetic support for Scirrotherium through one single synapomorphy, i.e. 94 presence of deep longitudinal depressions (LDs) in osteoderms. This is a distinctive feature 95 of S. carinatum but, in contrast, the LDs in S. hondaensis are relatively shallow, rather than 96 deep. Interestingly, this putative synapomorphy is actually shared by K. paranensis. Góis 97 explained the insufficient phylogenetic resolution in his analysis for Scirrotherium using 98 the argument of fragmentary character of the fossil specimens of S. hondaensis, although in 99
Recommended publications
  • Chronology, Causes and Progression of the Messinian Salinity Crisis
    letters to nature the cause, and the effects, of the isolation of the Mediterranean; the two basic explanations are (1) a large glacio-eustatic sea-level drop, Chronology, causes and related to expanding polar ice volume6, and (2) orogenic uplift accompanied by gravity-driven sliding of large nappe complexes in progression of the the Gibraltar arc7. Until now, correlations of stable-isotope (d18O and d13C) records from open-ocean sequences to the Messinian Messinian salinity crisis event stratigraphy of the Mediterranean have been ambiguous because of the absence of a reliable time frame for the MSC. The W. Krijgsman*, F. J. Hilgen², I. Raf®³, F. J. Sierro§ establishment of astronomical polarity timescales for the past & D. S. Wilsonk 10 Myr (refs 3, 11) provided a signi®cant advance in dating the * Paleomagnetic Laboratory ``Fort Hoofddijk'', Utrecht University, geological record and promised a solution for the MSC controver- Budapestlaan 17, 3584 CD Utrecht, The Netherlands sies. Unfortunately, the Mediterranean-based astronomical polarity ² Department of Geology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, timescale showed a gap during much of the Messinian (6.7±5.3 Myr The Netherlands ago)3, related to the presence of less-favourable sediments and the ³ Dipartimento di Scienze della Terra, UniversitaÁ ``G. D'Annunzio'', notoriously complex geological history of the Mediterranean in Campus Universitario, Via dei Vestini 31, 66013 Chieti Scalo, Italy this time interval. However, the classic Messinian sediments § Department de
    [Show full text]
  • Studies on Continental Late Triassic Tetrapod Biochronology. I. the Type Locality of Saturnalia Tupiniquim and the Faunal Succession in South Brazil
    Journal of South American Earth Sciences 19 (2005) 205–218 www.elsevier.com/locate/jsames Studies on continental Late Triassic tetrapod biochronology. I. The type locality of Saturnalia tupiniquim and the faunal succession in south Brazil Max Cardoso Langer* Departamento de Biologia, FFCLRP, Universidade de Sa˜o Paulo (USP), Av. Bandeirantes 3900, 14040-901 Ribeira˜o Preto, SP, Brazil Received 1 November 2003; accepted 1 January 2005 Abstract Late Triassic deposits of the Parana´ Basin, Rio Grande do Sul, Brazil, encompass a single third-order, tetrapod-bearing sedimentary sequence that includes parts of the Alemoa Member (Santa Maria Formation) and the Caturrita Formation. A rich, diverse succession of terrestrial tetrapod communities is recorded in these sediments, which can be divided into at least three faunal associations. The stem- sauropodomorph Saturnalia tupiniquim was collected in the locality known as ‘Waldsanga’ near the city of Santa Maria. In that area, the deposits of the Alemoa Member yield the ‘Alemoa local fauna,’ which typifies the first association; includes the rhynchosaur Hyperodapedon, aetosaurs, and basal dinosaurs; and is coeval with the lower fauna of the Ischigualasto Formation, Bermejo Basin, NW Argentina. The second association is recorded in deposits of both the Alemoa Member and the Caturrita Formation, characterized by the rhynchosaur ‘Scaphonyx’ sulcognathus and the cynodont Exaeretodon, and correlated with the upper fauna of the Ischigualasto Formation. Various isolated outcrops of the Caturrita Formation yield tetrapod fossils that correspond to post-Ischigualastian faunas but might not belong to a single faunal association. The record of the dicynodont Jachaleria suggests correlations with the lower part of the Los Colorados Formation, NW Argentina, whereas remains of derived tritheledontid cynodonts indicate younger ages.
    [Show full text]
  • Neogene Stratigraphy of the Langenboom Locality (Noord-Brabant, the Netherlands)
    Netherlands Journal of Geosciences — Geologie en Mijnbouw | 87 - 2 | 165 - 180 | 2008 Neogene stratigraphy of the Langenboom locality (Noord-Brabant, the Netherlands) E. Wijnker1'*, T.J. Bor2, F.P. Wesselingh3, D.K. Munsterman4, H. Brinkhiris5, A.W. Burger6, H.B. Vonhof7, K. Post8, K. Hoedemakers9, A.C. Janse10 & N. Taverne11 1 Laboratory of Genetics, Wageningen University, Arboretumlaan 4, 6703 BD Wageningen, the Netherlands. 2 Prinsenweer 54, 3363 JK Sliedrecht, the Netherlands. 3 Naturalis, P.O. Box 9517, 2300 RA Leiden, the Netherlands. 4 TN0 B&0 - National Geological Survey, P.O. Box 80015, 3508 TA Utrecht, the Netherlands. 5 Palaeocecology, Inst. Environmental Biology, Laboratory of Palaeobotany and Palynology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands. 6 P. Soutmanlaan 18, 1701 MC Heerhugowaard, the Netherlands. 7 Faculty Earth and Life Sciences, Vrije Universiteit, de Boelelaan 1085, 1081 EH Amsterdam, the Netherlands. 8 Natuurmuseum Rotterdam, P.O. Box 23452, 3001 KL Rotterdam, the Netherlands. 9 Minervastraat 23, B 2640 Mortsel, Belgium. 10 Gerard van Voornestraat 165, 3232 BE Brielle, the Netherlands. 11 Snipweg 14, 5451 VP Mill, the Netherlands. * corresponding author. Email: [email protected] Manuscript received: February 2007; accepted: March 2008 Abstract The locality of Langenboom (eastern Noord-Brabant, the Netherlands), also known as Mill, is famous for its Neogene molluscs, shark teeth, teleost remains, birds and marine mammals. The stratigraphic context of the fossils, which have been collected from sand suppletions, was hitherto poorly understood. Here we report on a section which has been sampled by divers in the adjacent flooded sandpit 'De Kuilen' from which the Langenboom sands have been extracted.
    [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]
  • Revised Stratigraphy of Neogene Strata in the Cocinetas Basin, La Guajira, Colombia
    Swiss J Palaeontol (2015) 134:5–43 DOI 10.1007/s13358-015-0071-4 Revised stratigraphy of Neogene strata in the Cocinetas Basin, La Guajira, Colombia F. Moreno • A. J. W. Hendy • L. Quiroz • N. Hoyos • D. S. Jones • V. Zapata • S. Zapata • G. A. Ballen • E. Cadena • A. L. Ca´rdenas • J. D. Carrillo-Bricen˜o • J. D. Carrillo • D. Delgado-Sierra • J. Escobar • J. I. Martı´nez • C. Martı´nez • C. Montes • J. Moreno • N. Pe´rez • R. Sa´nchez • C. Sua´rez • M. C. Vallejo-Pareja • C. Jaramillo Received: 25 September 2014 / Accepted: 2 February 2015 / Published online: 4 April 2015 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2015 Abstract The Cocinetas Basin of Colombia provides a made exhaustive paleontological collections, and per- valuable window into the geological and paleontological formed 87Sr/86Sr geochronology to document the transition history of northern South America during the Neogene. from the fully marine environment of the Jimol Formation Two major findings provide new insights into the Neogene (ca. 17.9–16.7 Ma) to the fluvio-deltaic environment of the history of this Cocinetas Basin: (1) a formal re-description Castilletes (ca. 16.7–14.2 Ma) and Ware (ca. 3.5–2.8 Ma) of the Jimol and Castilletes formations, including a revised formations. We also describe evidence for short-term pe- contact; and (2) the description of a new lithostratigraphic riodic changes in depositional environments in the Jimol unit, the Ware Formation (Late Pliocene). We conducted and Castilletes formations. The marine invertebrate fauna extensive fieldwork to develop a basin-scale stratigraphy, of the Jimol and Castilletes formations are among the richest yet recorded from Colombia during the Neogene.
    [Show full text]
  • Tetrapod Biostratigraphy and Biochronology of the Triassic–Jurassic Transition on the Southern Colorado Plateau, USA
    Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 242–256 www.elsevier.com/locate/palaeo Tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau, USA Spencer G. Lucas a,⁎, Lawrence H. Tanner b a New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104-1375, USA b Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA Received 15 March 2006; accepted 20 June 2006 Abstract Nonmarine fluvial, eolian and lacustrine strata of the Chinle and Glen Canyon groups on the southern Colorado Plateau preserve tetrapod body fossils and footprints that are one of the world's most extensive tetrapod fossil records across the Triassic– Jurassic boundary. We organize these tetrapod fossils into five, time-successive biostratigraphic assemblages (in ascending order, Owl Rock, Rock Point, Dinosaur Canyon, Whitmore Point and Kayenta) that we assign to the (ascending order) Revueltian, Apachean, Wassonian and Dawan land-vertebrate faunachrons (LVF). In doing so, we redefine the Wassonian and the Dawan LVFs. The Apachean–Wassonian boundary approximates the Triassic–Jurassic boundary. This tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau confirms that crurotarsan extinction closely corresponds to the end of the Triassic, and that a dramatic increase in dinosaur diversity, abundance and body size preceded the end of the Triassic. © 2006 Elsevier B.V. All rights reserved. Keywords: Triassic–Jurassic boundary; Colorado Plateau; Chinle Group; Glen Canyon Group; Tetrapod 1. Introduction 190 Ma. On the southern Colorado Plateau, the Triassic– Jurassic transition was a time of significant changes in the The Four Corners (common boundary of Utah, composition of the terrestrial vertebrate (tetrapod) fauna.
    [Show full text]
  • Latest Pliocene Northern Hemisphere Glaciation Amplified by Intensified Atlantic Meridional Overturning Circulation
    ARTICLE https://doi.org/10.1038/s43247-020-00023-4 OPEN Latest Pliocene Northern Hemisphere glaciation amplified by intensified Atlantic meridional overturning circulation ✉ Tatsuya Hayashi 1 , Toshiro Yamanaka 2, Yuki Hikasa3, Masahiko Sato4, Yoshihiro Kuwahara1 & Masao Ohno1 1234567890():,; The global climate has been dominated by glacial–interglacial variations since the intensifi- cation of Northern Hemisphere glaciation 2.7 million years ago. Although the Atlantic mer- idional overturning circulation has exerted strong influence on recent climatic changes, there is controversy over its influence on Northern Hemisphere glaciation because its deep limb, North Atlantic Deep Water, was thought to have weakened. Here we show that Northern Hemisphere glaciation was amplified by the intensified Atlantic meridional overturning cir- culation, based on multi-proxy records from the subpolar North Atlantic. We found that the Iceland–Scotland Overflow Water, contributing North Atlantic Deep Water, significantly increased after 2.7 million years ago and was actively maintained even in early stages of individual glacials, in contrast with late stages when it drastically decreased because of iceberg melting. Probably, the active Nordic Seas overturning during the early stages of glacials facilitated the efficient growth of ice sheets and amplified glacial oscillations. 1 Division of Environmental Changes, Faculty of Social and Cultural Studies, Kyushu University, 744 Motooka, Fukuoka 819-0395, Japan. 2 School of Marine Resources and Environment, Tokyo University of Marine Science and Technology, 4-5-7 Konan, Tokyo 108-8477, Japan. 3 Department of Earth Sciences, Graduate School of Natural Science and Technology, Okayama University, 1-1, Naka 3-chome, Tsushima, Okayama 700-8530, Japan. 4 Department of Earth ✉ and Planetary Science, The University of Tokyo, 7-3-1 Hongo, Tokyo 113-0033, Japan.
    [Show full text]
  • Episodes 149 September 2009 Published by the International Union of Geological Sciences Vol.32, No.3
    Contents Episodes 149 September 2009 Published by the International Union of Geological Sciences Vol.32, No.3 Editorial 150 IUGS: 2008-2009 Status Report by Alberto Riccardi Articles 152 The Global Stratotype Section and Point (GSSP) of the Serravallian Stage (Middle Miocene) by F.J. Hilgen, H.A. Abels, S. Iaccarino, W. Krijgsman, I. Raffi, R. Sprovieri, E. Turco and W.J. Zachariasse 167 Using carbon, hydrogen and helium isotopes to unravel the origin of hydrocarbons in the Wujiaweizi area of the Songliao Basin, China by Zhijun Jin, Liuping Zhang, Yang Wang, Yongqiang Cui and Katherine Milla 177 Geoconservation of Springs in Poland by Maria Bascik, Wojciech Chelmicki and Jan Urban 186 Worldwide outlook of geology journals: Challenges in South America by Susana E. Damborenea 194 The 20th International Geological Congress, Mexico (1956) by Luis Felipe Mazadiego Martínez and Octavio Puche Riart English translation by John Stevenson Conference Reports 208 The Third and Final Workshop of IGCP-524: Continent-Island Arc Collisions: How Anomalous is the Macquarie Arc? 210 Pre-congress Meeting of the Fifth Conference of the African Association of Women in Geosciences entitled “Women and Geosciences for Peace”. 212 World Summit on Ancient Microfossils. 214 News from the Geological Society of Africa. Book Reviews 216 The Geology of India. 217 Reservoir Geomechanics. 218 Calendar Cover The Ras il Pellegrin section on Malta. The Global Stratotype Section and Point (GSSP) of the Serravallian Stage (Miocene) is now formally defined at the boundary between the more indurated yellowish limestones of the Globigerina Limestone Formation at the base of the section and the softer greyish marls and clays of the Blue Clay Formation.
    [Show full text]
  • S40645-019-0306-X.Pdf
    Isaji et al. Progress in Earth and Planetary Science (2019) 6:60 Progress in Earth and https://doi.org/10.1186/s40645-019-0306-x Planetary Science RESEARCH ARTICLE Open Access Biomarker records and mineral compositions of the Messinian halite and K–Mg salts from Sicily Yuta Isaji1* , Toshihiro Yoshimura1, Junichiro Kuroda2, Yusuke Tamenori3, Francisco J. Jiménez-Espejo1,4, Stefano Lugli5, Vinicio Manzi6, Marco Roveri6, Hodaka Kawahata2 and Naohiko Ohkouchi1 Abstract The evaporites of the Realmonte salt mine (Sicily, Italy) are important archives recording the most extreme conditions of the Messinian Salinity Crisis (MSC). However, geochemical approach on these evaporitic sequences is scarce and little is known on the response of the biological community to drastically elevating salinity. In the present work, we investigated the depositional environments and the biological community of the shale–anhydrite–halite triplets and the K–Mg salt layer deposited during the peak of the MSC. Both hopanes and steranes are detected in the shale–anhydrite–halite triplets, suggesting the presence of eukaryotes and bacteria throughout their deposition. The K–Mg salt layer is composed of primary halites, diagenetic leonite, and primary and/or secondary kainite, which are interpreted to have precipitated from density-stratified water column with the halite-precipitating brine at the surface and the brine- precipitating K–Mg salts at the bottom. The presence of hopanes and a trace amount of steranes implicates that eukaryotes and bacteria were able to survive in the surface halite-precipitating brine even during the most extreme condition of the MSC. Keywords: Messinian Salinity Crisis, Evaporites, Kainite, μ-XRF, Biomarker Introduction hypersaline condition between 5.60 and 5.55 Ma (Manzi The Messinian Salinity Crisis (MSC) is one of the most et al.
    [Show full text]
  • The Less-Splendid Isolation of the South American Continent
    news and update ISSN 1948-6596 commentary The less-splendid isolation of the South American continent Only few biogeographic scenarios capture the im- lower Central America (Costa Rica) and South agination as much as the closure of the Isthmus of America (northern Colombia), and that some Panama. The establishment of this connection snapping shrimp populations were already split ended the “splendid isolation” of the South Amer- long before the Isthmus had finally closed (most ican continent (Simpson 1980), a continent that between 7–10 mya but some >15 mya). Next to had been unconnected to any other land mass for this, several papers showed that plants also mi- over 50 million years. When the Isthmus rose out grated between North and South America prior to of the water some 3 million years ago (mya) the the closure of the Isthmus (e.g., Erkens et al. 2007, Great American Biotic Interchange started. Since Bacon et al. 2013), although for plants it is difficult terrestrial biotic interchange was no longer to rule out that this happened via long-distance blocked by the Central American Seaway, dispersal. Thus, the new findings of Montes and (asymmetrical) invasion of taxa across this new colleagues fit much better with a wealth of evi- land bridge transformed biodiversity in North as dence from the biological realm that has been well as South America (Leigh et al. 2014). Or so amassed over the last years, than the old model of the story goes. a relatively rapid rise of the Isthmus. A recent paper by Montes et al. (2015) casts If the land-bridge was available much earli- further serious doubt on this scenario from a geo- er to many terrestrial organisms, the question that logical perspective.
    [Show full text]
  • Geology and Vertebrate Paleontology of Western and Southern North America
    OF WESTERN AND SOUTHERN NORTH AMERICA OF WESTERN AND SOUTHERN NORTH PALEONTOLOGY GEOLOGY AND VERTEBRATE Geology and Vertebrate Paleontology of Western and Southern North America Edited By Xiaoming Wang and Lawrence G. Barnes Contributions in Honor of David P. Whistler WANG | BARNES 900 Exposition Boulevard Los Angeles, California 90007 Natural History Museum of Los Angeles County Science Series 41 May 28, 2008 Paleocene primates from the Goler Formation of the Mojave Desert in California Donald L. Lofgren,1 James G. Honey,2 Malcolm C. McKenna,2,{,2 Robert L. Zondervan,3 and Erin E. Smith3 ABSTRACT. Recent collecting efforts in the Goler Formation in California’s Mojave Desert have yielded new records of turtles, rays, lizards, crocodilians, and mammals, including the primates Paromomys depressidens Gidley, 1923; Ignacius frugivorus Matthew and Granger, 1921; Plesiadapis cf. P. anceps; and Plesiadapis cf. P. churchilli. The species of Plesiadapis Gervais, 1877, indicate that Member 4b of the Goler Formation is Tiffanian. In correlation with Tiffanian (Ti) lineage zones, Plesiadapis cf. P. anceps indicates that the Laudate Discovery Site and Edentulous Jaw Site are Ti2–Ti3 and Plesiadapis cf. P. churchilli indicates that Primate Gulch is Ti4. The presence of Paromomys Gidley, 1923, at the Laudate Discovery Site suggests that the Goler Formation occurrence is the youngest known for the genus. Fossils from Member 3 and the lower part of Member 4 indicate a possible marine influence as Goler Formation sediments accumulated. On the basis of these specimens and a previously documented occurrence of marine invertebrates in Member 4d, the Goler Basin probably was in close proximity to the ocean throughout much of its existence.
    [Show full text]
  • Carlos Fernando De Gracia
    Carlos Fernando De Gracia Institutional Address Department of Paleontology, Faculty of Earth Sciences, Geography and Astronomy University of Vienna Althanstraße 14 / 2A323 1090 Vienna, Austria Phone number Office: +43-1-4277-53530 Personal: +43-677-63736404 e-Mail [email protected] ____________________________________________________________________________ Personal Information ORCID id 0000-0003-0637-3302 Date of birth 2th March, 1986 Place of birth Panama City, Panama Nationality. Panamanian ____________________________________________________________________________ Formal Education 2015 - 2017 Master in Geology, specific field: Geobiology Charles University in Prague, Prague, Czech Republic Thesis: Fossil Istiophorids (Perciformes, Istiophoridae) from the Chagres Formation, Panama Year of degree: 2017 Advisor: Tomás Přikryl Co-advisor: Carlos Alberto Jaramillo Scholarship from: Ministry of Education, Youth and Sports, Czech Republic 2004 - 2010 B. Sc. in Biology, specific field: animal biology Universidad de Panamá, Panama City, Panama Thesis: Structure of benthic communities on the pacific coast of Panama and Costa Rica during the formastion of Central American Ithmus, Year of degree: 2010 Advisors: Aaron O’Dea, Luis D´Croz 2014 - 2015 Improvement Course in Czech Language Charles University in Prague, Prague, Czech Republic Scholarship from: Ministry of Education, Youth and Sports ____________________________________________________________________________ Complementary Education 2011 - 2011 Postgraduate Course in Tropical
    [Show full text]