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JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
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A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans Robert W. BOESSENECKER Department of Geology, University of Otago, 360 Leith Walk, P.O. Box 56, Dunedin, 9054 (New Zealand) and Department of Earth Sciences, Montana State University 200 Traphagen Hall, Bozeman, MT, 59715 (USA) and University of California Museum of Paleontology 1101 Valley Life Sciences Building, Berkeley, CA, 94720 (USA) [email protected] Boessenecker R. W. 2013. — A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans. Geodiversitas 35 (4): 815-940. http://dx.doi.org/g2013n4a5 ABSTRACT e newly discovered Upper Miocene to Upper Pliocene San Gregorio assem- blage of the Purisima Formation in Central California has yielded a diverse collection of 34 marine vertebrate taxa, including eight sharks, two bony fish, three marine birds (described in a previous study), and 21 marine mammals. Pinnipeds include the walrus Dusignathus sp., cf. D. seftoni, the fur seal Cal- lorhinus sp., cf. C. gilmorei, and indeterminate otariid bones. Baleen whales include dwarf mysticetes (Herpetocetus bramblei Whitmore & Barnes, 2008, Herpetocetus sp.), two right whales (cf. Eubalaena sp. 1, cf. Eubalaena sp. 2), at least three balaenopterids (“Balaenoptera” cortesi “var.” portisi Sacco, 1890, cf. Balaenoptera, Balaenopteridae gen. et sp. indet.) and a new species of rorqual (Balaenoptera bertae n. sp.) that exhibits a number of derived features that place it within the genus Balaenoptera. is new species of Balaenoptera is relatively small (estimated 61 cm bizygomatic width) and exhibits a comparatively nar- row vertex, an obliquely (but precipitously) sloping frontal adjacent to vertex, anteriorly directed and short zygomatic processes, and squamosal creases. -
Anatomical Description and Phylogenetic Analysis of Miocene
Southern Methodist University SMU Scholar Collection of Engaged Learning Engaged Learning 4-15-2013 Anatomical description and phylogenetic analysis of Miocene beaked whale from the East African Rift Valley, Kenya Andrew Lin Southern Methodist University, [email protected] Follow this and additional works at: https://scholar.smu.edu/upjournal_research Part of the Earth Sciences Commons Recommended Citation Lin, Andrew, "Anatomical description and phylogenetic analysis of Miocene beaked whale from the East African Rift alV ley, Kenya" (2013). Collection of Engaged Learning. 10. https://scholar.smu.edu/upjournal_research/10 This document is brought to you for free and open access by the Engaged Learning at SMU Scholar. It has been accepted for inclusion in Collection of Engaged Learning by an authorized administrator of SMU Scholar. For more information, please visit http://digitalrepository.smu.edu. 1 Anatomical description and phylogenetic analysis of Miocene beaked whale from the East African Rift Valley, Kenya by Andrew Lin Undergraduate Senior Thesis Huffington Department of Earth Sciences Southern Methodist University Dallas, TX 75275 Abstract This study compares the anatomy of a Miocene whale fossil found in Kenya to that of modern and other fossil beaked whales in order to identify it using phylogenetic analysis. The specimen is a partial skull and lacks diagnostic features present in the posterior regions of the skull, but a parsimony analysis based on available characters determined the whale is likely linked to modern Mesoplodon and Hyperoodon. Identification of this specimen is necessary for biogeographical purposes and other investigations using the fossil as a marker for the paleocoastline. Furthermore, this whale is an important and unique tool that can be used to study the development of the East African Rift. -
Beaked Whale Mysteries Revealed by Seafloor Fossils Trawled Off South Africa
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Open Marine Archive 140 South African Journal of Science 104, March/April 2008 Research Letters Beaked whale mysteries revealed by seafloor fossils trawled off South Africa a b Giovanni Bianucci *, Klaas Post and c Olivier Lambert An unexpectedly large number of well-preserved fossil ziphiid (beaked whale) skulls trawled from the seafloor off South Africa significantly increases our knowledge of this cetacean family. The Fig. 1. Map of the South African coast showing localities where ziphiid skulls were eight new genera and ten new species more than double the known trawled by fishing and research vessels. diversity of fossil beaked whales and represent more than one-third of this family (fossil and extant). A cladistic parsimony analysis based on 18 cranial characters suggested that some of these fossil taxa belong to the three extant ziphiid subfamilies, whereas others might represent extinct ziphiid lineages. Such high fossil ziphiid diversity might be linked to the upwelling system and the resulting high productivity of the Benguela Current, which has been in place and influenced conditions of the shallower waters along the south- west coast of South Africa and Namibia since the Middle Miocene. Both fossil and extant South African beaked whale faunas show a wide range in body size, which is probably related to different dietary niches and to wide exploration of the water column. More- over, most South African fossil ziphiids share two morphological traits with extant species, which indicates that some of the behaviours associated with these traits had likely already developed during the Neogene: 1) the absence of functional maxillary teeth—providing clear evidence of suction feeding; and 2) the heavy ossification of the rostrum in specimens assumed to represent adult males—a feature which likely helps prevent injury and damage on impact during male–male fighting. -
Caviziphius Altirostris, a New Beaked Whale from the Miocene Southern North Sea Basin
Giovanni Bianucci 1 & Klaas Post 2 1 Università di Pisa 2 Natuurhistorisch Museum Rotterdam Caviziphius altirostris, a new beaked whale from the Miocene southern North Sea basin Bianucci, G. & Post, K., 2005 - Caviziphius altirostris, a new beaked whale from the Miocene southern North Sea basin - DEINSEA 11: 1-6 [ISSN 0923-9308]. Published 29 December 2005 An odontocete cranium from Miocene deposits in northern Belgium is examined and referred to Caviziphius altirostris, a new genus and species of beaked whale. In the general architecture of its vertex and closed mesorostral canal, Caviziphius resembles the fossil genera Ziphirostrum and Choneziphius, but differs from all known ziphiids by a very deep excavated prenarial basin with a semicircular outline in lateral view. This peculiar cranial architecture of Caviziphius might indicate an advanced and efficient mechanism of sound production in this fossil ziphiid. Keywords: Cetacea, Ziphiidae, Miocene, North Sea, new taxon Correspondence: G. Bianucci, Dipartimento di Scienze della Terra, Università di Pisa, Via S. Maria, 5356126 Pisa, Italy; e-mail: [email protected]. K. Post (to whom correspondence should be addressed), Natuurhistorisch Museum Rotterdam, P.O. Box 23452, 3001 KL Rotterdam, the Netherlands; e-mail: [email protected] INTRODUCTION cranium, here described and referred to a new Miocene and Pliocene marine deposits from genus and species. the southern North Sea Basin are a very impor- The anatomical terminology utilized follows tant source of fossil cetaceans (odontocetes and Heyning (1989) and measurements were made mysticetes). Most specimens originate from the according the methods used by Moore (1963). Antwerp area in Belgium, but important fossils have also been collected from the Netherlands SYSTEMATIC PALEONTOLOGY and the North Sea. -
Systematics and Phylogeny of the Fossil Beaked Whales Ziphirostrum Du Bus, 1868 and Choneziphius Duvernoy, 1851 (Mammalia, Cetac
Systematics and phylogeny of the fossil beaked whales Ziphirostrum du Bus, 1868 and Choneziphius Duvernoy, 1851 (Mammalia, Cetacea, Odontoceti), from the Neogene of Antwerp (North of Belgium) Olivier LAMBERT Institut royal des Sciences naturelles de Belgique, Département de Paléontologie, rue Vautier, 29, B-1000 Brussels (Belgium) [email protected] Lambert O. 2005. — Systematics and phylogeny of the fossil beaked whales Ziphirostrum du Bus, 1868 and Choneziphius Duvernoy, 1851 (Mammalia, Cetacea, Odontoceti), from the Neogene of Antwerp (North of Belgium). Geodiversitas 27 (3) : 443-497. ABSTRACT A systematic revision of the fossil beaked whales (Cetacea, Odontoceti, Ziphiidae) Ziphirostrum du Bus, 1868 and Choneziphius Duvernoy, 1851 from the Neogene of Antwerp (Belgium, southern margin of the North Sea Basin) is undertaken. It is based on several rostra and partial skulls from the collection of the Institut royal des Sciences naturelles de Belgique. From the previous conclusions about those taxa, dating from the beginning of the 20th century and suggesting only one species in each genus, Mioziphius ( Ziphirostrum) belgicus and Choneziphius planirostris, the following modifica- tions are proposed. The genus Ziphirostrum includes three species: Z. mar- ginatum, Z. turniense, and Z. recurvus n. comb. Basicranial fragments and teeth of Z. marginatum are described for the first time. Besides the most com- mon species Choneziphius planirostris, the species C. macrops is identified from Antwerp and the east coast of North America. A new genus and species KEY WORDS Mammalia, Beneziphius brevirostris n. gen., n. sp. is described on the basis of two specimens Cetacea, characterized by a short and pointed rostrum. Two partial skulls are placed in Odontoceti, Ziphiidae aff. -
Agraulos Longicephalus and Proampyx? Depressus (Trilobita) from the Middle Cambrian of Bornholm, Denmark
Content, vol. 63 63 · 2015 Bulletin of the Geological Society Denmark · Volume Thomas Weidner & Arne Thorshøj Nielsen: Agraulos longicephalus and Proampyx? depressus (Trilobita) from the Middle Cambrian of Bornholm, Denmark ................ 1 Jens Morten Hansen: Finally, all Steno’s scientific papers translated from Latin into English. Book review of: Kardel. T. & Maquet, P. (eds) 2013: Nicolaus Steno. Biography and Original Papers of a 17th Century Scientist. Springer-Verlag, Berlin, Heidelberg, 739 pp ..................................................................................... 13 Lars B. Clemmensen, Aslaug C. Glad, Kristian W. T. Hansen & Andrew S. Murray: Episodes of aeolian sand movement on a large spit system (Skagen Odde, Denmark) and North Atlantic storminess during the Little Ice Age ....................... 17 Mette Olivarius, Henrik Friis, Thomas F. Kokfelt & J. Richard Wilson: Proterozoic basement and Palaeozoic sediments in the Ringkøbing–Fyn High characterized by zircon U–Pb ages and heavy minerals from Danish onshore wells ........................................................................................................ 29 Richard Pokorný, Lukáš Krmíček & Uni E. Árting: The first evidence of trace fossils and pseudo-fossils in the continental interlava volcaniclastic sediments on the Faroe Islands .............................................................................................. 45 Thomas Weidner, Gerd Geyer, Jan Ove R. Ebbestad & Volker von Seckendorff: Glacial erratic boulders from Jutland, Denmark, -
The Upper Miocene Deurne Member of the Diest
GEOLOGICA BELGICA (2020) 23/3-4: 219-252 The upper Miocene Deurne Member of the Diest Formation revisited: unexpected results from the study of a large temporary outcrop near Antwerp International Airport, Belgium Stijn GOOLAERTS1,*, Jef DE CEUSTER2, Frederik H. MOLLEN3, Bert GIJSEN3, Mark BOSSELAERS1, Olivier LAMBERT1, Alfred UCHMAN4, Michiel VAN HERCK5, Rieko ADRIAENS6, Rik HOUTHUYS7, Stephen LOUWYE8, Yaana BRUNEEL5, Jan ELSEN5 & Kristiaan HOEDEMAKERS1 1 OD Earth & History of Life, Scientific Heritage Service and OD Natural Environment, Royal Belgian Institute of Natural Sciences, Belgium; [email protected]; [email protected]; [email protected]; [email protected]. 2 Veldstraat 42, 2160 Wommelgem, Belgium; [email protected]. 3 Elasmobranch Research Belgium, Rehaegenstraat 4, 2820 Bonheiden, Belgium; [email protected]; [email protected]. 4 Faculty of Geography and Geology, Institute of Geological Sciences, Jagiellonian University, Gronostajowa 3a, 30-387 Kraków, Poland; [email protected]. 5 Department of Earth & Environmental Sciences, KU Leuven, Belgium; [email protected]; [email protected]; [email protected]. 6 Q Mineral, Heverlee, Belgium; [email protected]. 7 Independent consultant, Halle, Belgium; [email protected]. 8 Department of Geology, Campus Sterre, S8, Krijgslaan 281, 9000 Gent, Belgium; [email protected]. * corresponding author. ABSTRACT. A 5.50 m thick interval of fossiliferous intensely bioturbated -
Crown Beaked Whale Fossils from the Chepotsunai Formation (Latest Miocene) of Tomamae Town, Hokkaido, Japan
Palaeontologia Electronica palaeo-electronica.org Crown beaked whale fossils from the Chepotsunai Formation (latest Miocene) of Tomamae Town, Hokkaido, Japan Yoshihiro Tanaka, Mahito Watanabe, and Masaichi Kimura ABSTRACT In the last decades, our knowledge of ziphiid evolution has increased dramatically. However, their periotic morphology is still poorly known. A fossil ziphiid (TTM-1) includ- ing the periotic, bulla, isolated polydont teeth and vertebrae from the Chepotsunai For- mation (latest Miocene) of Tomamae Town, Hokkaido, Japan, is identified as a member of a clade with crown ziphiids of Bianucci et al. (2016) by having three periotic synapo- morphies; a posteriorly wide posterior process, transversely thick anterior process, and laterally elongated lateral process. The specimen adds morphological information of the periotic. Among the Ziphiidae from the stem to crown, the periotic morphologies were changed to having a more robust anterior process, wider anterior bullar facet and posterior process. The crown Ziphiidae shares a feature; enlarged medial tubercle on the anterior process. Among the crown Ziphiidae, TTM-1 does not have a swollen medial tubercle not like Tasmacetus, Nazcacetus and others. This new morphological information might represent useful future phylogenetic comparisons. Yoshihiro Tanaka. Osaka Museum of Natural History, Nagai Park 1-23, Higashi-Sumiyoshi-ku, Osaka, 546- 0034, Japan. [email protected] Hokkaido University Museum, Kita 10, Nishi 8, Kita-ku, Sapporo, Hokkaido 060-0810 Japan, Numata Fossil Museum, 2-7-49, Minami 1, Numata town, Hokkaido 078-2225 Japan Mahito Watanabe. AIST, Geological Survey of Japan, Research Institute for Geology and Geoinformation, Central 7, 1-1-1 Higashi, Tsukuba, Ibaraki, 305-8567 Japan. -
Origin and Evolution of Large Brains in Toothed Whales
WellBeing International WBI Studies Repository 12-2004 Origin and Evolution of Large Brains in Toothed Whales Lori Marino Emory University Daniel W. McShea Duke University Mark D. Uhen Cranbrook Institute of Science Follow this and additional works at: https://www.wellbeingintlstudiesrepository.org/acwp_vsm Part of the Animal Studies Commons, Other Animal Sciences Commons, and the Other Ecology and Evolutionary Biology Commons Recommended Citation Marino, L., McShea, D. W., & Uhen, M. D. (2004). Origin and evolution of large brains in toothed whales. The Anatomical Record Part A: Discoveries in Molecular, Cellular, and Evolutionary Biology, 281(2), 1247-1255. This material is brought to you for free and open access by WellBeing International. It has been accepted for inclusion by an authorized administrator of the WBI Studies Repository. For more information, please contact [email protected]. Origin and Evolution of Large Brains in Toothed Whales Lori Marino1, Daniel W. McShea2, and Mark D. Uhen3 1 Emory University 2 Duke University 3 Cranbrook Institute of Science KEYWORDS cetacean, encephalization, odontocetes ABSTRACT Toothed whales (order Cetacea: suborder Odontoceti) are highly encephalized, possessing brains that are significantly larger than expected for their body sizes. In particular, the odontocete superfamily Delphinoidea (dolphins, porpoises, belugas, and narwhals) comprises numerous species with encephalization levels second only to modern humans and greater than all other mammals. Odontocetes have also demonstrated behavioral faculties previously only ascribed to humans and, to some extent, other great apes. How did the large brains of odontocetes evolve? To begin to investigate this question, we quantified and averaged estimates of brain and body size for 36 fossil cetacean species using computed tomography and analyzed these data along with those for modern odontocetes. -
New Discoveries of Fossil Toothed Whales from Peru: Our Changing Perspective of Beaked Whale and Sperm Whale Evolution
Quad. Mus. St. Nat. Livorno, 23: 13-27 (2011) DOI code: 10.4457/musmed.2010.23.13 13 New discoveries of fossil toothed whales from Peru: our changing perspective of beaked whale and sperm whale evolution OLIVIER LAMBERT1 SUMMARY: Following the preliminary description of a first fossil odontocete (toothed whale) from the Miocene of the Pisco Formation, southern coast of Peru, in 1944, many new taxa from Miocene and Pliocene levels of this formation were described during the 80’s and 90’s, (families Kentriodontidae, Odobenocetopsidae, Phocoenidae, and Pontoporiidae). Only one Pliocene Ziphiidae (beaked whale) and one late Miocene Kogiidae (dwarf sperm whale) were defined. Modern beaked whales and sperm whales (Physeteroidea = Kogiidae + Physeteridae) share several ecological features: most are predominantly teuthophagous, suction feeders, and deep divers. They further display a highly modified cranial and mandibular morphology, including tooth reduction in both groups, high vertex and sexually dimorphic mandibular tusks in ziphiids, and development of a vast supracranial basin in physeteroids. New discoveries from the Miocene of the Pisco Formation enrich the fossil record of ziphiids and physeteroids and shed light on various aspects of their evolution. From Cerro Colorado, a new species of the ziphiid Messapicetus lead to the description of features previously unknown in fossil members of the family: association of complete upper and lower tooth series with tusks, hypothetical sexual dimorphism in the development of the tusks, skull anatomy of a calf... A new small ziphiid from Cerro los Quesos, Nazcacetus urbinai, is characterized by the reduction of the dentition: a pair of apical mandibular tusks associated to vestigial postapical teeth, likely hold in the gum. -
Rostral Densification in Beaked Whales: Diverse Processes for A
C. R. Palevol 10 (2011) 453–468 Contents lists available at ScienceDirect Comptes Rendus Palevol www.sciencedirect.com General palaeontology, systematics and evolution (Vertebrate palaeontology) Rostral densification in beaked whales: Diverse processes for a similar pattern La densification du rostre des baleines à bec : des processus variés pour un résultat similaire Olivier Lambert a,∗,b, Vivian de Buffrénil a, Christian de Muizon a a Département histoire de la terre, Muséum national d’histoire naturelle, UMR 7207 (paléobiodiversité et paléoenvironnements), (MNHN, CNRS, UPMC), CP 38, 57, rue Cuvier, 75005 Paris, France b Département de paléontologie, institut royal des sciences naturelles de Belgique, Bruxelles, Belgium article info abstract Article history: As compared to other odontocetes (toothed whales), the rostrum of beaked whales (family Received 24 September 2010 Ziphiidae) often displays extensive changes in the shape, thickness, and density of its con- Accepted after revision 21 March 2011 stituent bones. Previous morphological observations suggested that these modifications Available online 31 May 2011 appeared in parallel in different ziphiid lineages. However, very few data were available on the compactness and histology of these rostral bones, which precluded the study of the pro- Written on invitation of the Editorial Board. cesses at work for the development of such structures, as well as the interpretation of their functional implications. In this work we review the bibliographic data on the anatomy of the Keywords: ziphiid rostrum and we add new observations on adults of several extinct and extant taxa. Odontoceti Ziphiidae These observations are based on CT scans and transverse histological sections. Our results Beaked whales confirm that different bones (vomer, mesethmoid, premaxilla, maxilla) are involved in the Pachyostosis various morphologies displayed by ziphiid rostra.