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  • evolution  (2)
  • 551.7  (1)
  • ARGOS Location-only transmitter ST10; Dallmann Laboratory; DATE/TIME; JUB1996; JUB1996_sel_u_m_01; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Positioning type/details; Southern Ocean - Atlantic Sector  (1)
  • ARGOS Location-only transmitter ST10; Dallmann Laboratory; DATE/TIME; JUB1996; JUB1996_sel_u_m_03; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Positioning type/details; Southern Ocean - Atlantic Sector  (1)
Document type
Keywords
Language
Years
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Journal of mammalian evolution 1 (1993), S. 227-254 
    ISSN: 1573-7055
    Keywords: enamel microstructure ; evolution ; incisors ; Mixodontia ; Rodentia
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Incisor enamel microstructure proved to be a very effective tool for assessment of phylogenetic relationships among the Rodentia. Pauciserial and multiserial Schmelzmuster are clearly distinct by structural characters such as orientation of interprismatic matrix, presence or absence of transition zones between Hunter-Schreger bands (HSB), inclination of HSB, enamel thickness, and others. Pauciserial HSB are structurally very close to the earliest known mammalian HSB found in Paleocene arctocyonids. Biomechanical arguments and outgroup comparison with mixodontians indicate that the pauciserial Schmelzmuster is a symplesiomorphy of the Rodentia. Transitional stages from pauciserial to multiserial Schmelzmuster were observed in middle Eocene ctenodactyloids and from pauciserial to uniserial in middle to late Eocene anomalurids. The multiserial Schmelzmuster is considered a synapomorphy of the Hystricognathi, ctenodactylids, and pedetids. Schmelzmuster evolution reflects the early dichotomy of the Rodentia: In the Asian ctenodactyloid lineage a multiserial Schmelzmuster evolved once and in the North American/European ischyromyoid lineage a uniserial Schmelzmuster developed several times convergently. The pauci- to uniserial Schmelzmuster of the anomalurids excludes a close relationship to the phiomyids, because the ctenodactyloid-phiomyid lineage is characterized by the development of a multiserial Schmelzmuster.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Journal of mammalian evolution 2 (1994), S. 117-131 
    ISSN: 1573-7055
    Keywords: enamel microstructure ; evolution ; Chaetomys ; incisors ; Caviomorpha
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract We have studied the incisor enamel microstructure ofChaetomys subspinosus and other possibly closely related caviomorph rodents.Chaetomys subspinosus lacks the important synapomorphy of the Octodontoidea, reactangular plate-like interprismatic matrix (IPM) in the portio interna (PI) of the incisor Schmelzmuster. Therefore its transfer from the Erethizontidae to the Echimyidae, as proposed by Patterson and Wood (Bull. Mus. Comp. Zool. 149, 371–543, 1982) based on retention of dP4, is contested. The parallel to acute angular IPM in the PI ofChaetomys and the Erethizontidae is a symplesiomorphy and does not indicate close relationship. Contrary to previous claims, a posterior carotid foramen is also retained inChaetomys. Chaetomys is characterized by an unusual thin enamel which is considered primitive after outgroup comparison. Therefore, it is proposed to leaveChaetomys in the monospecific erethizontid subfamily Chaetomyinae, until additional information on the species is available.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2021-06-05
    Description: Drei Auerochsenskelette (Bos primigenius) und ein Bisonskelett (Bison priscus) aus dem Jungpleistozän bzw. Holozän Deutschlands werden osteologisch beschrieben. Gattungsunterschiede an den Langknochen werden an den mit Hilfe des Schädels sicher bestimmten Skelettfunden auf ihre Zuverlässigkeit hin überprüft. In die Untersuchung wird Vergleichsmaterial von Bos primigenius und Bison priscus aus dem Pleistozän von England sowie von Bison div. sp. aus Nordamerika einbezogen. Schlüsselmerkmale für eine Unterscheidung von Bos primigenius und Bison priscus existieren nicht. Die in einer früheren Arbeit an Material aus den Schottern der nördlichen Oberrheinebene (Martin 1987) ausgearbeiteten Merkmalskombinationen konnten als brauchbar bestätigt werden, wobei sich erneut zeigte, daß sehr zierliche Knochen in ihren Merkmalsausprägungen abweichen können. Die Unterscheidungsmerkmale lassen sich generell auch auf den nordamerikanischen Bison antiquus und Bison bison erfolgreich anwenden, sofern die Knochen in derselben Größenklasse wie die von Bison priscus liegen.
    Description: research
    Keywords: 551.7 ; VAR 000 ; Glazialgeologie ; bos primigenius ; bison priscus ; holocene ; upper pleistocene ; upper rhine valley ; northern german hills ; rhine westphalian basin ; north rhine-westphalia ; hesse ; biometry ; ruminantia ; skeletons ; skulls ; extremities ; humerus ; radius ; femur ; tibia ; lower saxony ; taxonomy
    Language: German
    Type: article , publishedVersion
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  • 4
    Publication Date: 2023-07-15
    Keywords: ARGOS Location-only transmitter ST10; Dallmann Laboratory; DATE/TIME; JUB1996; JUB1996_sel_u_m_01; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Positioning type/details; Southern Ocean - Atlantic Sector
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 5
    Publication Date: 2023-07-15
    Keywords: ARGOS Location-only transmitter ST10; Dallmann Laboratory; DATE/TIME; JUB1996; JUB1996_sel_u_m_03; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Positioning type/details; Southern Ocean - Atlantic Sector
    Type: Dataset
    Format: text/tab-separated-values, 548 data points
    Location Call Number Limitation Availability
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