Adolf Seilacher (1925–2014) Palaeontologist Who Pioneered Analysis of Trace Fossils
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Planispiral Burrows from a Recent Lacustrine Beach, Gander Lake, Newfoundland
Planispiral Burrows from a Recent Lacustrine Beach, Gander Lake, Newfoundland ROBERT B. M AC NAUGHTON Geological Survey of Canada, 3303 – 33 Street NW, Calgary, Alberta T2L 2A7 Canada; e-mail: [email protected] MacNaughton, Robert B. 2003. Planispiral burrows from a Recent lacustrine beach, Gander Lake Newfoundland. Canadian Field-Naturalist 117(4): 577-581. Simple horizontal, planispiral burrows occur in Recent beach sediments on the south shore of Gander Lake, Newfoundland. The burrows apparently represent deposit feeding, possibly by an arthropod. This occurrence extends the known environ- mental range of such traces into lacustrine settings and illustrates that such behaviour is not exclusive to marine settings. Key Words: ichnology, lacustrine, Recent, palaeoecology, Newfoundland. Ichnology is the study of the physical records of The beach on which the burrows were observed is behaviour, including, for example, tracks, trails, bur- approximately 90 m east of the mouth of Fifteen Mile rows, and borings (Bromley 1990). Studies are under- Brook (Figure 1). At the time of study, the beach was taken both in fossil and Recent contexts (palichnol- approximately 3 m wide by 24 m long. It passed on ogy and neoichnology, respectively). Fossilised traces the landward side into forest-covered glacio-fluvial are referred to as “trace fossils” or “ichnofossils” and sand and gravel (Figure 1), from which it was prob- are classified using Linnean binominal nomenclature. ably, in part, derived (cf., Batterson and Vatcher 1991). Although much ichnological research is focused on the Small driftwood logs were scattered over the beach. fossil record, neoichnology can provide crucial data The beach surface consisted of damp to wet (but not when interpreting ancient behaviours (e.g., Schäfer water-saturated), muddy to silty, fine- to medium- 1972; Chamberlain 1975; Ratcliffe and Fagerstrom grained sand containing local concentrations of finely 1980; Metz 1987). -
Yale Earth & Planetary Sciences News
YALE EARTH & PLANETARY SCIENCES NEWS Yale University I Department of Earth & Planetary Sciences FALL NEWSLETTER 2020 Since our last newsletter (in Chair’s Letter 2018) we have added two new faculty, Assistant Profes- sors Juan Lora and Lidya Dear Friends, Family and Tarhan. Juan studies plan- Alumni of Yale Earth etary atmospheres and & Planetary Sciences, climates, and is one of the principal investigators on the Surely one of the first upcoming NASA Dragonfly things you’ll notice, espe- Mission to the Saturnian moon cially you alumni, is that Juan Lora, Assistant Titan. Titan is one of the big- the department changed Professor gest moons in our solar sys- its name. On July 1, 2020 tem, is the only one with a thick atmosphere made the department went from of mostly nitrogen, and has a methane cycle similar Geology & Geophysics to Earth’s hydrological cycle, which carries water to Earth & Planetary Sci- and heat around our planet. Juan also examines Dave Bercovici ences. This change has how a warming climate on Earth affects water been brewing for decades, transport through atmospheric rivers. through many cycles of discussions, polls, and debates, and was finally Lidya Tarhan works on made official this year. This is not the first time ancient environments, and the department’s name has changed. Yale is one especially how the earliest of the first educational institutions in the country animal life, at and before the to teach the science of the Earth, starting in 1804 time of the Cambrian explo- with a single faculty member, Benjamin Silliman, as sion 540 million years ago, professor of Chemistry and Natural History. -
Hierarchical Random Walks in Trace Fossils and the Origin of Optimal Search Behavior
Hierarchical random walks in trace fossils and the origin of optimal search behavior David W. Simsa,b,c,1, Andrew M. Reynoldsd, Nicolas E. Humphriesa, Emily J. Southalla, Victoria J. Wearmoutha, Brett Metcalfee, and Richard J. Twitchettf aMarine Biological Association of the United Kingdom, Plymouth PL1 2PB, United Kingdom; bOcean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Waterfront Campus, Southampton SO14 3ZH, United Kingdom; cCentre for Biological Sciences, University of Southampton, Highfield Campus, Southampton SO17 1BJ, United Kingdom; dRothamsted Research, Harpenden, Hertfordshire AL5 2JQ, United Kingdom; eEarth and Climate Cluster, Faculty of Earth and Life Sciences, VU University Amsterdam, 1081 HV, Amsterdam, The Netherlands; and fDepartment of Earth Sciences, The Natural History Museum, London SW7 5BD, United Kingdom Edited by H. Eugene Stanley, Boston University, Boston, MA, and approved June 19, 2014 (received for review April 1, 2014) −μ Efficient searching is crucial for timely location of food and other “walk clusters” with no characteristic scale, such that P(l) ∼ l , resources. Recent studies show that diverse living animals use a with 1 < μ ≤ 3, where l is the move step length between turns and theoretically optimal scale-free random search for sparse resources μ the power-law exponent. Over many iterations, a Lévy walk will known as a Lévy walk, but little is known of the origins and evo- be distributed much further from its starting position than a lution of foraging behavior and the search strategies of extinct Brownian walk of the same length [hence is termed super- organisms. Here, using simulations of self-avoiding trace fossil trails, diffusive (8)], because small-step walk clusters are interspersed we show that randomly introduced strophotaxis (U-turns)—initiated by long “steps” to new locations, with this pattern repeating by obstructions such as self-trail avoidance or innate cueing—leads across all scales. -
A NEW METAZOAN from the MIDDLE CAMBRIAN of UTAH and the NATURE of the VETULICOLIA by DEREK E
[Palaeontology, Vol. 48, Part 4, 2005, pp. 681–686] RAPID COMMUNICATION A NEW METAZOAN FROM THE MIDDLE CAMBRIAN OF UTAH AND THE NATURE OF THE VETULICOLIA by DEREK E. G. BRIGGS*, BRUCES.LIEBERMAN , SUSAN L. HALGEDAHLà and RICHARD D. JARRARDà *Department of Geology and Geophysics, Yale University, PO Box 208109, New Haven, CT 06520-8109, USA; e-mail: [email protected] Department of Geology, University of Kansas, 1475 Jayhawk Boulevard, 120 Lindley Hall, Lawrence, KS 66045, USA àDepartment of Geology and Geophysics, University of Utah, 135 S. 1460 East, Salt Lake City, UT 84112, USA Typescript received 22 November 2004; accepted in revised form 24 March 2005 Abstract: A new metazoan, Skeemella clavula gen. et sp. arthropodan in character. The similarity of this fossil nov., is described from the Middle Cambrian Pierson Cove to vetulicolians throws hypotheses of their deuterostome Formation of the Drum Mountains, Utah, USA. Skeemella affinity into question and highlights their problematic sta- is similar to vetulicolians, but differs from other examples tus. of this group in the relative proportions of the anterior and posterior sections, the large number of divisions, and Key words: vetulicolian, Cambrian, deuterostome, arthro- the elongate bifid termination. The posterior section is pod. The very name vetulicolian conjures up creatures from species Banffia confusa, to erect a new class of stem-group another planet. These extraordinary fossils, with a head arthropods, the Vetulicolida. They argued that Banffia shield-like anterior and narrow segmented trunk-like pos- constricta from the Burgess Shale belongs to the same terior, are the latest Cambrian group to be accorded phy- class, extending its range to North America. -
Harry Whittington Dies 94
Published: 5:58PM BST 08 Aug 2010 Professor Harry Whittington Professor Harry Whittington, who died on June 20 aged 94, was the former Woodwardian Professor of Geology at Cambridge and the world’s leading authority on fossil trilobites; in later life he led painstaking research which revealed a “Cambrian explosion” and raised disturbing questions about the proCesses of evolution. Trilobites were hard-carapaced creatures, which thrived, in the Cambrian period, beginning 542 million years ago, until they died out nearly 300 million years later. Very distantly related to horseshoe crabs, they lived in the sea and crawled on land, evolving into more than 20,000 different species, ranging in size from a millimetre to nearly two feet. Many known species are ones which Whittington himself discovered on field trips around the world. Usually it is difficult to extract the fossils from the surrounding rock, but in the 1940s Whittington and his colleague Bill Evitt investigated beds in Virginia where the carapaces of the animals had been replaced by insoluble silica. By throwing samples into acid, they were able to recover thousands of perfect specimens, ranging from fully-grown adults to microscopic larvae. These fossils enabled Whittington, in a series of monographs published in the 1950s and 1960s, to revolutionize what we know about trilobites — how they grew from larva to maturity through successive molts, how they moved and articulated their bodies, and how they evolved and migrated. Later in his career, in 1966, Whittington was invited by the Canadian Geological Society to chair a group commissioned to examine the Burgess Shale deposits discovered by CD Walcott during the building of the Canadian Pacific Railway in 1909. -
The Discovery of a Paleodictyon-Like Trace Fossil from the Late Cambrian Machinchang Formation in Pulau Jemuruk, Langkawi, Malaysia
Geological Society of Malaysia, Bulletin 46 May 2003; pp. 421-424 The discovery of a Paleodictyon-like trace fossil from the Late Cambrian Machinchang Formation in Pulau Jemuruk, Langkawi, Malaysia MOHD SHAFEEA LEMAN School of Environmental Sciences and Natural Resources, Faculty of Science and Technology Universiti Kebangsaan Malaysia, 43600 Bangi, Selangor Abstract: Closely spaced polygonal Paleodictyon-like trace fossil was recently discovered in Late Cambrian Machinchang Formation at Pulau Jemuruk, Langkawi. Each polygon is bounded by six segments of ridges forming unique hexagonal framework. The Jemuruk fossil has an epi-relief origin, contrary to the hypo-relief burrow Paleodictyon. The Jemuruk trace fossils formed in relatively shallower marine environment compared with other known Paleodictyon. This study shows that the Kinneyia structure found in the same layer originated from these Paleodictyon-like trace fossils. Abstrak: Surihan berbentuk poligon menyerupai Paleodictyon telah ditemui dalam batuan Kambria Akhir Formasi Machinchang di Pulau Jemuruk, Langkawi. Setiap ruang fosil surih ini disempadani enam segmen permatang membentuk kerangka heksagon yang menarik. Fosil Jemuruk berasalan epi-jasatimbul manakala Paleodictyon adalah sejenis korekan hipo-jasatimbul. Fosil surih Jemuruk terbentuk pada sekitaran laut lebih cetek berbanding dengan Paleodictyon yang diketahui. Kajian juga menunjukkan bahawa struktur Kinneyia yang ditemui dalam lapisan yang sarna adalah berasal daripada fosil surih seakan Paleodictyon ini. INTRODUCTION the Tarutao Formation described (later) by Teroaka et al. (1982) from Ko Tarutao in southern Thailand. The later The Machinchang Formation is perhaps the best has a comparatively similar lithological sequence with the described Cambrian rock formation in Malaysia. Despite Machinchang Formation and is a northern extension of the being one of the oldest rock formation in the country, most Machinchang Formation beyond the Malaysia-Thailand of its rocks are neither strongly deformed nor highly border. -
THE SYNTHETIC THEORY of EVOLUTION DNA Makes RNA, RNA Makes Protein and Proteins Make Us
320 Chapter f THE AGE OF MAMMALS The Present is the Key to the Past: HUGH RANCE THE SYNTHETIC THEORY OF EVOLUTION DNA makes RNA, RNA makes protein and proteins make us. —Crick.1 f14 Genes, alleles < deoxyribonucleic acid > ...using the metaphor of computation to describe the role of genes is bad biology, for it implies an internal self-sufficiency of DNA. Even if we had the complete DNA sequence of an organism and unlimited computational power, we could not compute an organism, because an organism does not compute itself from its genes. (In fact, any computer that did as poor a job of computation as a genetic “program” does of an organism would immediately be thrown into the trash.) —Richard Lewontin The Triple Helix: Gene, Organism, and Environment, 2000.2 Mathematical population theorists Ronald Aylmer Fisher (The Genetical Theory of Natural Selection, 1930),3 John Burdon Sanderson Haldane (design disparaging: “[He has] an inordinate fondness for beetles.”),4 and Sewall Wright (conceiver of “adaptive landscapes”)5 were the principle forgers, during the period 1920-1950, of the modern theory of population genetics that unites previously warring concepts (Footnote f14.1) of Darwinian natural selection, which is decidedly nonrandom, that guides evolution incrementally (by gradual change) but rapidly by its recursiveness (the output of previous selection is input for subsequent selection), along paths to fitness, and the purely random nature (no inherent directionality, no predictability) of heredity by large sudden changes (saltations, hopeful monsters) that Mendelian rules suggested to some geneticists (principally, typologists William Bateson, Hugo de Vries, and Wilhelm Johannsen). -
Cambrian Substrate Revolution
Vol. 10, No. 9 September 2000 INSIDE • Research Grants, p. 12 • Section Meetings Northeastern, p. 16 GSA TODAY Southeastern, p. 18 A Publication of the Geological Society of America • Happy Birthday, NSF, p. 22 The Cambrian Substrate Revolution David J. Bottjer, Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0740, [email protected] James W. Hagadorn, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, [email protected] Stephen Q. Dornbos, Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0740, [email protected] ABSTRACT The broad marine ecological settings prevalent during the late Neo- proterozoic–early Phanerozoic (600–500 Ma) interval of early metazoan body plan origination strongly impacted the subsequent evolution and development of benthic metazoans. Recent work demonstrates that late Neoproterozoic seafloor sediment had well-developed microbial mats and poorly developed, vertically oriented bioturbation, thus producing fairly stable, relatively low water content substrates and a sharp water-sediment interface. Later in the Cambrian, seafloors with microbial mats became increasingly scarce in shallow-marine environments, largely due to the evolution of burrowing organisms with an increasing vertically oriented component to their bioturba- tion. The evolutionary and ecological effects of these substrate changes on Figure 1. Looping and meandering trace fossil Taphrhelminthopsis, made by a large Early Cambrian benthic metazoans, referred to as the bioturbator, on a bedding plane from Lower Cambrian Poleta Formation, White-Inyo Mountains, California. Such traces, consisting of a central trough between lateral ridges, occur in sandstones Cambrian substrate revolution, are deposited in shallow-marine environments. -
10 Ekdale & Gibert.Indd
SPANISH JOURNAL OF PALAEONTOLOGY Late Miocene deep-sea trace fossil associations in the Vera Basin, Almería, Southeastern Spain Allan A. EKDALE1* & Jordi M. de GIBERT2 1 Department of Geology and Geophysics, University of Utah, FASB 383, 115 South 1460 East, Salt Lake City, UT 84112- 0102, U.S.A.; [email protected] 2 Deceased (September 23, 2012) * Corresponding author Ekdale, A. & Gibert, J.M. 2014. Late Miocene deep-sea trace fossil associations in the Vera Basin, Almería, Southeastern Spain. [Asociaciones de trazas fósiles marinas profundas del Mioceno superior de la cuenca de Vera, Almería, Sureste de España]. Spanish Journal of Palaeontology, 29 (1), 95-104. Manuscript received 02 May 2013 © Sociedad Española de Paleontología ISSN 2255-0550 Manuscript accepted 12 September 2013 ABSTRACT RESUMEN The Vera Basin in southeastern Spain was a small, tectonically La Cuenca de Vera, en el sureste español, fue un pequeño active depocenter throughout the Miocene. In the early depocentro tectónicamente activo durante todo el Mioceno. Messinian, approximately 7.2 to 6.0 million years ago, A principios del Messiniense, hace aproximadamente 7,2- the basin received hemipelagic marl deposits that were 6,0 millones de años, la cuenca recibió depósitos margosos punctuated by turbidite events. Soles of thin, turbidite sand hemipelágicos, interrumpidos por episodios turbidíticos. beds preserve an abundance of pre-depositional graphoglyptid En la base de los niveles de arenas turbidíticas se conserva (agrichnial) burrows that represent diverse deep-sea una gran cantidad de grafoglíptidos pre-deposicionales ichnocoenoses, including Paleodictyon, Urohelminthoida (agrichnia) que representan diversas icnocenosis de aguas and Helminthorhaphe. Post-depositional feeding burrows, profundas, incluyendo Paleodictyon, Urohelminthoida including Ophiomorpha (created by crustaceans) and y Helminthorhaphe. -
A Solution to Darwin's Dilemma: Differential Taphonomy of Ediacaran and Palaeozoic Non-Mineralised Discoidal Fossils
Provided by the author(s) and NUI Galway in accordance with publisher policies. Please cite the published version when available. Title A Solution to Darwin's Dilemma: Differential Taphonomy of Ediacaran and Palaeozoic Non-Mineralised Discoidal Fossils Author(s) MacGabhann, Breandán Anraoi Publication Date 2012-08-29 Item record http://hdl.handle.net/10379/3406 Downloaded 2021-09-26T20:57:04Z Some rights reserved. For more information, please see the item record link above. A Solution to Darwin’s Dilemma: Differential taphonomy of Palaeozoic and Ediacaran non- mineralised discoidal fossils Volume 1 of 2 Breandán Anraoi MacGabhann Supervisor: Dr. John Murray Earth and Ocean Sciences, School of Natural Sciences, NUI Galway August 2012 Differential taphonomy of Palaeozoic and Ediacaran non-mineralised fossils Table of Contents List of Figures ........................................................................................................... ix List of Tables ........................................................................................................... xxi Taxonomic Statement ........................................................................................... xxiii Acknowledgements ................................................................................................ xxv Abstract ................................................................................................................. xxix 1. Darwin’s Dilemma ............................................................................................... -
Deep-Sea Trace Fossils in the West Crocker Formation, Sabah (Malaysia), and Their Palaeoenvironmental Significance Mazlan Madon
Bulletin of the Geological Society of Malaysia, Volume 71, May 2021, pp. 23 - 46 DOI: https://doi.org/10.7186/bgsm71202103 Deep-sea trace fossils in the West Crocker Formation, Sabah (Malaysia), and their palaeoenvironmental significance Mazlan Madon Malaysian Continental Shelf Project, National Security Council, Kuala Lumpur, Malaysia Author email address: [email protected] Abstract: In the “flysch” series of the West Crocker Formation (Eocene–Oligocene), Kota Kinabalu, Sabah, trace fossils are fairly common although not ubiquitous. The trace fossils commonly occur as hypichnial semi- or full-reliefs on the sole of thin turbiditic sandstone beds (mainly Bouma Tc division) in the thinly bedded heterolithic sandstone-mudstone facies interpreted as submarine fan lobe deposits. Their presence in mainly the thinly bedded facies of the fan system suggests preferential production and preservation in the fine-grained “distal” parts of the Crocker submarine fan system. Trace fossil assemblages characteristic of the Nereites ichnofacies indicate sedimentary environments mainly in bathyal to abyssal water depths (>2000 m). This ichnofacies is dominated by horizontal grazing, farming and feeding traces, ranging from solitary to branching tubular burrows (Ophiomorpha, Palaeophycus and Planolites) to meandering trails and tunnels (Nereites, Cosmorhaphe, Helminthopsis), as well as the spiriform burrows Spirophycus. Graphoglyptids are the most diagnostic of the Nereites ichnofacies, produced by sediment grazers and farmers (agrichnia) and often displaying intricate networks of mainly horizontal tunnels preserved as hypichnial semi-reliefs. They include the delicate spiral traces of Spirorhaphe, as well as the enigmatic hexagonal network burrow Paleodictyon. Other ichnogenera include Planolites, Thalassinoides and Ophiomorpha which are facies-crossing and not environment specific. -
A Mixed Assemblage of Deep-Sea and Shelf Trace Fossils from the Lower Cretaceous (Valanginian) Kamchia Formation in the Troyan Region, Central Fore-Balkan, Bulgaria
Annales Societatis Geologorum Poloniae (2003), vol. 73: 27-34. A MIXED ASSEMBLAGE OF DEEP-SEA AND SHELF TRACE FOSSILS FROM THE LOWER CRETACEOUS (VALANGINIAN) KAMCHIA FORMATION IN THE TROYAN REGION, CENTRAL FORE-BALKAN, BULGARIA Alfred UCHMAJV1 & Platon TCHOUMATCHENCO2, 1 Institute o f Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063 Kraków, Poland, e-mail: fred@ing. uj. edu.pl 2 Geological Institute, Bulgarian Academy o f Sciences, Acad. G. Boncev Str., Bl. 24, 1113 Sofia, Bulgaria, e-mail: platon@lark. vmei. acad. bg Uchman, A. & Tchoumatchenco, P., 2003. A mixed assemblage of deep-sea and shelf trace fossils from the Lower Cretaceous (Valanginian) Kamchia Formation in the Troyan region, central Fore-Balkan, Bulgaria. Annales Societatis Geologorum Poloniae, 73: 27-34. Abstract: Trace fossils collected from the best outcrop of the Kamchia Formation have been analysed. There are thirteen ichnotaxa (Curvolithus simplex, Gyrochorte isp., IHelminthoidichnites tenuis, Multina minima [second occurrence], Palaeophycus tubularis, ?Palaeophycus isp., Phycodes bilix, Phycosiphon incertum, Planolites cf. reinecki, Spongeliomorpha Ichevronensis, Squamodictyon tectiforme, Thalassinoides suevicus, Zoophycos isp.) representing different ethologic, toponomic and preservational types, and produced at different depths in the sediment. The ichnoassemblage contains a mixture of forms typical of flysch (Squamodictyon) and shelf deposits (Cun'olithus, Gyrochorte). Probably, sediments of the Kamchia Formation were deposited in an offshore or deeper basin with storm deposition of sand beds and background marly sedimentation. It is possible that storm currents transported trace makers of the shelf trace fossils to the deeper sea. It is not excluded that the trace maker of Gyrochorte migrated to the deep-sea after the Jurassic.