A New Eurypterid from the Saaremaa- (Oesel-) Beds in Estonia
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Hypothesis of Eurypterid Palaeoecology
Palaeogeography, Palaeoclimatology, Palaeoecology 311 (2011) 63–73 Contents lists available at SciVerse ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Testing the ‘mass-moult-mate’ hypothesis of eurypterid palaeoecology Matthew B. Vrazo ⁎, Simon J. Braddy Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, UK article info abstract Article history: The eurypterids (Arthropoda: Chelicerata), some of the earliest arthropods to undertake amphibious Received 6 May 2011 excursions onto land, are generally rare in the fossil record, but are sometimes found in great abundance, for Received in revised form 16 July 2011 example in the Late Silurian Bertie Group of New York State. The mass-moult-mate hypothesis has been Accepted 29 July 2011 proposed to explain such occurrences, whereby eurypterids undertook mass migrations into near shore Available online 5 August 2011 settings and lagoons to moult, mate and spawn, similar to the behaviour of living horseshoe crabs. This hypothesis is tested using measurements from over 600 Eurypterus specimens from three localities in the Keywords: Arthropod Bertie Group; Eurypterus remipes, from the Fiddlers Green Formation, and the slightly larger Eurypterus Exuvia lacustris, from the overlying Williamsville Formation. Disarticulation patterns support previous evidence for Taphonomy moulted assemblages. A significant predominance of female exuviae is noted at each locality, unlike studies on Biofacies modern Limulus populations. Therefore, a modified mass-mate-spawn-moult hypothesis is proposed here: Silurian males returned to deeper waters after mating, whereas females, having mated, remained at the breeding sites Eurypterus to deposit their eggs before moulting. After hatching, eurypterid larvae and juveniles remained in these spawning grounds until they matured and could move to deeper water, in comparison with Limulus. -
Description of the Hollidaysburg and Huntingdon Quadrangles
DESCRIPTION OF THE HOLLIDAYSBURG AND HUNTINGDON QUADRANGLES By Charles Butts INTRODUCTION 1 BLUE RIDGE PROVINCE topography are therefore prominent ridges separated by deep SITUATION The Blue Ridge province, narrow at its north end in valleys, all trending northeastward. The Hollidaysburg and Huntingdon quadrangles are adjoin Virginia and Pennsylvania, is over 60 miles wide in North RELIEF ing areas in the south-central part of Pennsylvania, in Blair, Carolina. It is a rugged region of hills and ridges and deep, The lowest point in the quadrangles is at Huntingdon, Bedford, and Huntingdon Counties. (See fig. 1.) Taken as narrow valleys. The altitude of the higher summits in Vir where the altitude of the river bed is about 610 feet above sea ginia is 3,000 to 5,700 feet, and in western North Carolina 79 level, and the highest point is the southern extremity of Brush Mount Mitchell, 6,711 feet high, is the highest point east of Mountain, north of Hollidaysburg, which is 2,520 feet above the Mississippi River. Throughout its extent this province sea level. The extreme relief is thus 1,910 feet. The Alle stands up conspicuously above the bordering provinces, from gheny Front and Dunning, Short, Loop, Lock, Tussey, Ter each of which it is separated by a steep, broken, rugged front race, and Broadtop Mountains rise boldly 800 to 1,500 feet from 1,000 to 3,000 feet high. In Pennsylvania, however, above the valley bottoms in a distance of 1 to 2 miles and are South Mountain, the northeast end of the Blue Ridge, is less the dominating features of the landscape. -
Tayside, Central and Fife Tayside, Central and Fife
Detail of the Lower Devonian jawless, armoured fish Cephalaspis from Balruddery Den. © Perth Museum & Art Gallery, Perth & Kinross Council Review of Fossil Collections in Scotland Tayside, Central and Fife Tayside, Central and Fife Stirling Smith Art Gallery and Museum Perth Museum and Art Gallery (Culture Perth and Kinross) The McManus: Dundee’s Art Gallery and Museum (Leisure and Culture Dundee) Broughty Castle (Leisure and Culture Dundee) D’Arcy Thompson Zoology Museum and University Herbarium (University of Dundee Museum Collections) Montrose Museum (Angus Alive) Museums of the University of St Andrews Fife Collections Centre (Fife Cultural Trust) St Andrews Museum (Fife Cultural Trust) Kirkcaldy Galleries (Fife Cultural Trust) Falkirk Collections Centre (Falkirk Community Trust) 1 Stirling Smith Art Gallery and Museum Collection type: Independent Accreditation: 2016 Dumbarton Road, Stirling, FK8 2KR Contact: [email protected] Location of collections The Smith Art Gallery and Museum, formerly known as the Smith Institute, was established at the bequest of artist Thomas Stuart Smith (1815-1869) on land supplied by the Burgh of Stirling. The Institute opened in 1874. Fossils are housed onsite in one of several storerooms. Size of collections 700 fossils. Onsite records The CMS has recently been updated to Adlib (Axiel Collection); all fossils have a basic entry with additional details on MDA cards. Collection highlights 1. Fossils linked to Robert Kidston (1852-1924). 2. Silurian graptolite fossils linked to Professor Henry Alleyne Nicholson (1844-1899). 3. Dura Den fossils linked to Reverend John Anderson (1796-1864). Published information Traquair, R.H. (1900). XXXII.—Report on Fossil Fishes collected by the Geological Survey of Scotland in the Silurian Rocks of the South of Scotland. -
Trip A2 Paleoecology and Taphonomy of Some Eurypterid-Bearing
Trip A2 Paleoecology and Taphonomy of Some Eurypterid-Bearing Horizons in the Finger Lakes Region of New York State STEPHEN M. MAYER 5475 East Lake Road, Romulus, NY 14541, USA INTRODUCTION The Upper Silurian Bertie Group in western and central New York State is famous for its eurypterid (Arthropoda: Chelicerata) Lagerstätten. From the earliest recognition of the genus Eurypterus by American zoologist James Ellsworth Dekay (1825), studies have concentrated on eurypterid growth and variation (see Andrews et al., 1974; Cuggy, 1994). More recent works have focused on ecdysis (Tetlie et al., 2008), and mating (Braddy, 2001; Vrazo and Braddy, 2011), as well as trace fossils and taphonomy (Vrazo et al., 2014, 2016, 2017, and Vrazo and Ciurca, 2018). Recurrent taphonomic patterns are recognized regardless of species with various hypotheses proposed to explain these occurrences. The purpose of this investigation is to provide an overview of the preservation patterns observed in the fossil record. The contortion of Eurypterus remipes and Erieopterus microphthalmus exuviae collected from different Finger Lake sites, as well as specimens held in the Samuel J. Ciurca Eurypterid Collection at Yale Peabody Museum of Natural History are interpreted to be the result of flexure of eurypterid exoskeletons by submarine paleocurrents. The present contribution and accompanying field guide review the facies and geological settings of the Bertie Group with an emphasis on eurypterid-bearing horizons in west central New York as well as a discussion of specific aspects of the preservation of these fossils. PALEOGEOGRAPHY AND PALEOENVIRONMENTAL SETTINGS Silurian stratigraphy and paleoenvironmental conditions of western and central New York State have been studied extensively by Rickard (1969, 1975), Ciurca (1973), Belak (1980), Hamell and Ciurca (1986), Brett et al. -
Description of the Niagara Quadrangle
DESCRIPTION OF THE NIAGARA QUADRANGLE. By E. M. Kindle and F. B. Taylor.a INTRODUCTION. different altitudes, but as a whole it is distinctly higher than by broad valleys opening northwestward. Across northwestern GENERAL RELATIONS. the surrounding areas and is in general bounded by well-marked Pennsylvania and southwestern New York it is abrupt and escarpments. i nearly straight and its crest is about 1000 feet higher than, and The Niagara quadrangle lies between parallels 43° and 43° In the region of the lower Great Lakes the Glaciated Plains 4 or 5 miles back from the narrow plain bordering Lake Erie. 30' and meridians 78° 30' and 79° and includes the Wilson, province is divided into the Erie, Huron, and Ontario plains From Cattaraugus Creek eastward the scarp is rather less Olcott, Tonawanda, and Lockport 15-minute quadrangles. It and the Laurentian Plateau. (See fig. 2.) The Erie plain abrupt, though higher, and is broken by deep, narrow valleys thus covers one-fourth of a square degree of the earth's sur extending well back into the plateau, so that it appears as a line face, an area, in that latitude, of 870.9 square miles, of which of northward-facing steep-sided promontories jutting out into approximately the northern third, or about 293 square miles, the Erie plain. East of Auburn it merges into the Onondaga lies in Lake Ontario. The map of the Niagara quadrangle shows escarpment. also along its west side a strip from 3 to 6 miles wide comprising The Erie plain extends along the base of the Portage escarp Niagara River and a small area in Canada. -
Growth and Variation in Eurypterus Remipes Dekay
Bull. geo!. Instn Univ. Upsala: N. S. 4, 6: 81-114, 1974 GROWTH AND VARIATION IN EURYPTERUS REMIPES DEKAY By H. E. Andrews, ]. C. Brower, S. ]. Gould, and R. A. Reyment Andrews, H. E., Brower, ]. C., Gould, S. ]., Reyment, R. A.: Growth and Variation in EurypteruJ remipes DeKay, Bull. geo!. Instn Univ. Upsala, Vol. N. S 4, pp. 81-114. Th e statistic al analysis of two subspecies of Eurypterus remipes shows that both of them display very high integratio:� among all measures considered. The prosomal set of variables are highly integrated with the body set. There is little allometry in bivariate growth sequences. As best known at the present time, trilobites show an analogous leve! of integration; there is therefore reason to suspect that the gr owth relationships here recorded are wide-spread among some arthropods. Ontogenetic growth is analysed for E. remipes remipes, after the establishment of growth stages by a stepwise multivariate technique. Canonical correlation is used to examine the pattern of integration between head and body. This is, again, exceptionally high. Other methods of multi variate statistics are applied the analysis of the underlying relationships between variables. The palaeoec ology of the Fiddlersto Gr een Member (Bertie Formation, Upper Silurian) is discussed. H. E. Andrews, Department of Geology, \'(/ellesley Colle�;e, \'(/ellesley, Mass., U.S.A., S. ]. Gould, Museum of Comparative Zoology, Harvard University, Cambridge, Mass., U.S.A., ]. C. Brower, Department of Geology, Syracuse University, U.S.A., R. A. Reyment, Paleontologiska Institutionen, Uppsala Unit;ersitet. Su,eden. INTRODUCTION remipes and the E. tetragonophthalmus of Fischer Ever smce Mitchill (1818) recorded the first de Waldheim (synonym E. -
Electronic Appendix
ELECTRONIC APPENDIX This is the Electronic Appendix to the article Babes in the wood – a unique window into sea scorpion ontogeny by James C. Lamsdell and Paul A. Selden Comprising the morphological character list and character matrix used in the phylogenetic analysis Character list 1. Angular projection on the anterior of the carapace: absent (0); present (1). 2. Anterior margin of carapace: unornamented (0); denticulate (1). 3. Carapace marginal rim: present (0); absent (1). 4. Carapace genal spines: present (0); absent (1). 5. Carapace shape: horseshoe or wide-horseshoe (0); semicircular (1); quadrate (2); trapezoidal (3); wide-rectangular (4); subquadrate (5); campanulate (6); parabolic (7); spatulate (8); triangular (9); long-rectangular (10). 6. Carapace genal facets: absent (0); present (1). 7. Angle of genal facets: low angle (0); high angle (1). 8. Lateral eye shape: crescentic (0); expanded (1). 9. Size of palpebral lobe: small (0); large (1); absent (2). 10. Lateral eye position: centrilateral (0); centrimesial (1); antelateral (2); central (3); antemesial (4). 11. Lateral eye abuts carapace margin: absent (0); present (1). 12. Lateral eyes associated with ophthalmic ridge: present (0); absent (1). 13. Suture on ventral plates: Eurypterus-type (0); Hughmilleria- or Hallipterus-type (1); Megalograptus-type (2); Erieopterus-type (3). 14. Transverse suture on ventral plates: present (0); absent (1). 15. Chelicerae: small (0); able to extend beyond marginal rim (1). 16. Form of cheliceral peduncle: approximately equal in length to fixed ramus (0); longer than fixed ramus (1). 1 17. Denticles on chela: absent (0); present, small, undifferentiated (1); present, large, differentiated (2). 18. Largest denticle medially on fixed ramus: erect (0); inclined (1); acute (2). -
Prehistoric Life in the National Parks Coloring Book
National Park Service PREHISTORIC LIFE IN U.S. Department of the Interior THE NATIONAL PARKS COLORING BOOK PREHISTORIC LIFE IN THE NATIONAL PARKS COLORING BOOK National Park Service, Geologic Resources Division, Paleontology Program https://www.nps.gov/subjects/fossils/index.htm DEDICATION This Prehistoric Life in the National Parks Coloring Book is dedicated to Georgia Hybels, a National Park Service geographer who shared her time to foster children’s interests in fossils, caves and national parks. PRECAMBRIAN “before the Cambrian” The Precambrian Eon is part of Earth’s history. It spans from approximately 4.6 billion years ago to 541 million years ago. This section includes a Precambrian life form found in some of our national parks in the United States. Collenia symmetrica is an early fossil. It shows layers of sand trapped by tiny organisms (mostly cyanobacteria) into mounds that we call stromatolites. Stromatolites are some of the earliest and most widespread forms of early prehistoric life. Fossils of Collenia have been found at Glacier National Park, Montana. PALEOZOIC ERA “ancient animal life” The Paleozoic Era is part of Earth’s history that spans approximately 541 million years ago to 252 million years ago. This era began with an explosion of new life. New and different ocean animals lived during the Cambrian. Over time, plants and animals evolved to live in the oceans and on land. The Paleozoic ends after a large die off (extinction) of many early lifeforms at the end of the Permian. This section includes some Paleozoic life which have been found in some of our national parks in the United States. -
A New Carcinosomatid Eurypterid from the Upper Silurian of Northern Vietnam
A NEW CARCINOSOMATID EURYPTERID FROM THE UPPER SILURIAN OF NORTHERN VIETNAM by SIMON J. BRADDY, PAUL A. SELDEN and DOAN NHAT TRUONG ABSTRACT. A new carcinosomatid eurypterid, Rhinocarcinosoma dosonensis sp. nov., and Hughmilleria sp., are described from the Do Son Formation of the Do Son Peninsula, northern Vietnam. R. dosonensis is characterized by podomere 7 of prosomal appendage VI produced into an anterodistal spine, a metastoma with a cordate posterior margin, and an indented opisthosomal differentiation (i.e. preabdomen-postabdomen margin is concave). The Do Son Formation was originally interpreted as Late Devonian (Givetian/Frasnian) in age but the unit containing the eurypterid assemblage is now considered much older (Late Silurian). A deltaic palaeoenvironmental setting is interpreted from biotic associations and sedimentological evidence. KEY WORDS: chelicerate, eurypterid, Carsinosomatidae, Silurian, Vietnam, stratigraphy. THE Do Son Formation is almost entirely restricted in exposure to the Do Son Peninsula, a 4-km projection into the Gulf of Bac Bo (Tonkin), around 13 km south-east of Hai Phong in northern Vietnam (Text-fig. 1). It is approximately 400 m thick but its detailed stratigraphy remains debated. NguyenDinh Hoe (pers. comm. 1991) suggested that it may consist of three members: a 100-200-m-thick lower member of yellow-grey, massive, cross-bedded sandstones, a 100-m-thick middle member of pale red, cross-bedded sandstones interbedded with light grey-green siltstones and clay lenses, and a 150-m-thick upper member of light-green sandstones, siltstones, clays and shales. These siliciclastic deposits generally show a moderate (10-20°) dip to the south-east, but there seem to be local changes in dip direction, possibly due to faults. -
Eurypteridsofdev145kjel.Pdf
LIBRARY OF THE UNIVERSITY OF ILLINOIS AT URBANA-CH/^PAIGN 550.5n CM GEOLOGY UN/VERSITYOF ILLINOIS LIBRARY ATURBANA-CHAMPAIGM GEOLOGY ¥ K 50.5 r !s FIELDIANA • GEOLOGY Published by CHICAGO NATURAL HISTORY MUSEUM Volume 14 April 26, 1961 No. 5 Eurypterids of the Devonian Holland Quarry Shale of Ohio Erik N. Kjellesvig-Waering Research Associate, Department op Geology In contrast to the Silurian, the North American Devonian de- posits have not yielded a rich fauna of eurypterids, although the list of known species is continuously growing. The occurrence of euryp- terids in the Holland Quarry shale, a lens locally underlying the Syl- vania sandstone at the base of the Devonian in Lucas County, Ohio (see Carman, 1960), adds materially to our relatively meager knowl- edge of Devonian forms in North America. The eurypterids in this Lower Devonian deposit are preserved as patches of integument up to four inches in diameter, although most patches cover no more than one or two inches. The preserva- tion of these fragments is excellent, and permits study of minute details in structure and ornamentation. The eurypterids are inti- mately associated with numerous fishes and land plants in a dark gray to black bituminous shale with numerous single grains of coarse, round, frosted quartz sand, and clusters of these sand grains in pock- ets, along with small light-gray mud pellets (phosphatic?), some sul- phur specks, selenite crystals, pyrite and coaly or carbonized streaks which probably represent mineralized plants. The fishes included are pteraspids, cyathaspids and arthrodires (see Denison, 1960). The pterygotids are by far the most common eurypterids present. -
Review of Fossil Collections in Scotland Review of Fossil Collections in Scotland
Detail of the Upper Devonian fishHoloptychius from Dura Den, Fife. © Perth Museum & Art Gallery, Perth & Kinross Council Review of Fossil Collections in Scotland Review of Fossil Collections in Scotland Contents Introduction 3 Background 3 Aims of the Collections Review 4 Methodology 4 Terminology 5 Summary of fossil material 6 Influences on collections 14 Collections by region Aberdeen and North East 17 Elgin Museum (Moray Society) 18 Falconer Museum (Moray Council) 21 Stonehaven Tolbooth Museum 23 The Discovery Centre (Live Life Aberdeenshire) 24 Arbuthnot Museum (Live Life Aberdeenshire) 27 Zoology Museum (University of Aberdeen Museums) 28 Meston Science Building (University of Aberdeen Museums) 30 Blairs Museum 37 Highlands and Islands 38 Inverness Museum and Art Gallery (High Life Highland) 39 Nairn Museum 42 West Highland Museum (West Highland Museum Trust) 44 Brora Heritage Centre (Brora Heritage Trust) 45 Dunrobin Castle Museum 46 Timespan (Timespan Heritage and Arts Society) 48 Stromness Museum (Orkney Natural History Society) 50 Orkney Fossil and Heritage Centre 53 Shetland Museum and Archives (Shetland Amenity Trust) 56 Bute Museum (Bute Museum Trust) 58 Hugh Miller’s Birthplace Cottage and Museum (National Trust for Scotland) 59 Treasures of the Earth 62 Staffin Dinosaur Museum 63 Gairloch Museum (Gairloch & District Heritage Company Ltd) 65 Tayside, Central and Fife 66 Stirling Smith Art Gallery and Museum 67 Perth Museum and Art Gallery (Culture Perth and Kinross) 69 The McManus: Dundee’s Art Gallery and Museum (Leisure -
Its Position Within the Adelophthalmidae Tollerton, 1989 by O
bulletin de l'institut royal des sciences naturelles de belgique sciences de la terre, 76: 79-90, 2006 bulletin van het koninklijk belgisch instituut voor natuurwetenschappen aardwetenschappen, 76: 79-90, 2006 A reappraisal of Eurypterus dumonti Stainier, 1917 and its position within the Adelophthalmidae Tollerton, 1989 by O. Erik TETLIE & Peter VAN ROY Tetlie, O.E. & Van Roy, P., 2006 — A reappraisal of Eurypterus prétées ici comme des "dumb-hells" (cfr. Briggs & Wilby 1996), dumonti Stainier, 1917 and its position within the Adelophthalmidae résultant d'action bactérielle avant la fossilisation. Ces structures in¬ Tollerton, 1989. Bulletin de l'Institut royal des Sciences naturelles diquent que le fossile n'est pas une exuvie. L'interprétation d'un de Belgique, Sciences de la Terre 76: 79-90, 6 figs., Brussels, April 15, nombre d'autres caractéristiques diffère aussi de celle de la description 2006-ISSN 0374-6291. originale. Des lignes de descendance possible du clade Adelophthalmus sont identifiées, et la proximité (l'A. dumonti à A. imhofi (République Tchèque) et à A. moyseyi (Royaume-Uni) est suggérée. Abstract Mots-clefs: Eurypterida, appendices, 'dumb-bells', Belgique, terrain houiller. The Carboniferous eurypterid Eurypterus dumonti Stainier, 1917 from Mechelen-aan-de-Maas (Maasmechelen). Belgium is redescribed and assigned to the genus Adelophthalmus. It is diagnosed as having a Introduction raised triangle of unknown function, dorsally on opisthosomal segment 7 and a carapace articulating laterally against the second opisthosomal segment. Earlier assignments ofthis species to the genus Unionopterus, Eurypterids are a diverse group of Palaeozoic, aquatic based on the carapace shape fïgured in the original description chelicerates (Stainier 1917), are incorrect and the existence of a Carboniferous ranging from the Upper Ordovician eurypterid with the characteristics described for Unionopterus must be (Tollerton 2004) to the Upper Permian (Plotnick questioned.