Die zu den Sirenia, oder Seekühen, zählende Gattung Halitherium ist mit Arten aus dem Obereozän bis Untermiozän bekannt. Obwohl Halitherium als monophyletisch angesehen wird, bestätigen alle bisherigen phylogenetischen Analysen die Paraphylie dieser Gruppe. Auch die auf Halitherium basierende nur fossil bekannte Unterfamilie Halitheriinae ist paraphyletisch und umfasst wiederum fast ausnahmslos paraphyletische Gattungen. Der Fokus liegt auf der Typusart H. schinzii. Deren Holotyp, ein Premolar, wird als undiagnostisch definiert und infolgedessen H. schinzii als nomen dubium eingestuft. Die Neubeschreibung sämtlicher dieser Art zugeordneter Skelettreste liefert neue morphologische Daten. So kann die Hypothese von zwei sympatrisch vorkommenden Morphospezies im Unteroligozän Zentraleuropas auf Basis mehrerer unterscheidender Merkmale gestützt werden. Für die Verwandtschaftsanalyse der „Halitherium“ traditionell zugeordneten Arten und die Ermittlung ihrer phylogenetischen Stellung innerhalb der Ordnung Sirenia finden strenge kladistische Prinzipien Berücksichtigung. Eine revidierte, ergänzte und erweiterte Merkmalsmatrix stellt dabei den bisher größten morphologischen Datensatz über Sirenia dar. Die phylogenetischen Analysen zeigen, dass die „Halitherium“ Arten keine monophyletische Gruppe bilden. Im Zuge dieser systematisch-taxonomischen Revision werden die „Halitheriinae“ eingezogen und vier neue Gattungen aufgestellt. Des Weiteren wird eine neue Klassifikation der Sirenia vorgeschlagen, in der eine konsequente Unterscheidung zwischen einer paraphyletischen Stammgruppe und einer monophyletischen Kronengruppe Anwendung findet. Diese Studie liefert neue Daten über die Diversität und Biogeographie von Sirenen. Die herausragendsten Ergebnisse sind zum einen die Revision einer der zweifelhaftesten Sirenia Gruppen, die „Halitheriinae“. Zum anderen wird für den Ursprung der Kronengruppensirenen ein eher unteroligozäner statt eozäner Zeitpunkt postuliert. / The genus Halitherium includes a number of fossil sirenian species, or sea cows, ranging from the late Eocene to early Miocene. Although Halitherium is assumed to be monophyletic, all previous phylogenetic analyses reveal this group to be paraphyletic. As such, the exclusively extinct subfamily Halitheriinae based on Halitherium is paraphyletic comprising mainly genera that are invariably paraphyletic as well. The focus lies on the type species H. schinzii and the morphological basis for its establishment. The holotype, a single premolar, is considered non-diagnostic, which resulted in the recognition of this taxon name as a nomen dubium. Abundant skeletal material originally assigned to “H. schinzii” is re-described providing new data on the morphology of this sirenian. In this process, the hypothesis of two sympatric morphospecies in the lower Oligocene of Central Europe is corroborated by a suite of distinguishing characters. For the analysis of the interrelationships of the species traditionally assigned to “Halitherium”, and the identification of their phylogenetic position within the order Sirenia, robust cladistic principles are applied. A revised, supplemented and extended data matrix represents the hitherto largest data set on Sirenia based on morphological characters. The phylogenetic analyses show that the “Halitherium” species do not form a monophyletic group. In the course of this systematic and taxonomic revision the “Halitheriinae” are refuted and four new genera are established. Furthermore, a new systematic framework is introduced for Sirenia primarily distinguishing between a paraphyletic stem group and a monophyletic crown group. This study provides new data on the past sirenian diversity and biogeography. The most important results are that one of the most disputed sirenian groups, the “Halitheriinae”, is revised, and that the divergence time of crown group sirenians is estimated as early Oligocene rather than Eocene.

The latest Eocene and Oligocene was a time of marked paleoenvironmental change in Taranaki Basin, involving a transition from the accumulation of coal measures and inner shelf deposits to the development of upper bathyal environments. Up until the end of the Early Oligocene (Lower Whaingaroan Stage) Taranaki Basin had an extensional tectonic setting. Marine transgression culminated in the accumulation of condensed facies of the Matapo Sandstone Member of the lower part of the Ngatoro Group. During the Late Oligocene (Upper Whaingaroan Stage) Taranaki Basin's tectonic setting changed to one of crustal shortening with basement overthrusting westward into the basin on Taranaki Fault. The major part of the Ngatoro Group in thickness, including the Tariki Sandstone Member, Otaraoa Formation, Tikorangi Formation and Taimana Formation, accumulated in response to this change in tectonic setting. Various methods of stratigraphic and sedimentological characterisation have been undertaken to evaluate the stratigraphy of the Ngatoro Group. Wireline log records have been calibrated through particle sizing and carbonate digestion of well cuttings. A suite of wireline motifs have been defined for formations and members of the Ngatoro Group. The integration with other lithological and paleoenvironmental data sources has helped to better define the Late Eocene - Oligocene stratigraphy and sedimentary facies for eastern Taranaki Basin margin. U-Pb geochronology by laser ablation inductively coupled plasma-mass spectrometry (LA-ICP-MS) has been used to determine detrital ages for over 350 zircons from 13 samples of Late Eocene - Oligocene sandstone samples in eastern Taranaki Basin and correlative onshore North Island units. The spread of ages (1554 - 102 Ma) and the proportion of ages in particular age bands integrated with modal petrography data have aided provenance evaluation. A range of source rocks contributed to the Late Eocene - Oligocene sedimentary units analysed, mainly the Waipapa Terrane (Early Permian to Late Jurassic) as shown by 206Pb/238U zircon ages and the abundance of fine-grained sedimentary rock fragments observed in samples. The Median Batholith (i.e. Darran/Median Suite and Separation Point Suite) is also identified as a significant source, indicated by Early Triassic to Early Jurassic and Early Cretaceous 206Pb/238U zircon ages and an abundance of quartz in samples. Other minor sources identified include Murihiku and Caples Terranes, Rakaia Sub-terrane and possibly the Karamea Batholith. The Tariki Sandstone and the Hauturu Sandstone have the same source, with the main 206Pb/238U zircon ages of aggregated samples (124 - 116 Ma and 121 Ma, respectively) consistent with a Separation Point Suite/Median Batholith (124 - 116 Ma) source. Derivation of sediments from a landmass that existed to the east and southeast of the Wellington area has been inferred for the Late Eocene - Oligocene units, with subsequent migration of sediments northward into Taranaki Basin and the Waikato Region (i.e. Te Kuiti Group depocentre) via longshore drift. New provenance data have been used to revise understanding about the development of eastern Taranaki Basin margin through the Late Eocene to earliest Miocene. Three new paleogeography maps are presented for the Runangan (Late Eocene), Lower Whaingaroan (Early Oligocene) and Upper Whaingaroan (early-mid-Oligocene). New paleogeography interpretations illustrate a dramatic change in the basin development between Matapo Sandstone (Lower Whaingaroan) and Tariki Sandstone (Upper Whaingaroan) deposition, consistent with an Upper Whaingaroan age for the start of reverse movement on Taranaki Fault.

The Rodent Hill Locality is a fossil-bearing site that is part of the Cypress Hills Formation, and is located roughly 15 km northwest of the town of Eastend, Saskatchewan. A number of fossil mammal and other vertebrate taxa are present at Rodent Hill; the primary objective of this project was to identify the fossil rodents of the families Sciuridae, Aplodontidae, Castoridae, Heliscomyidae, Heteromyidae, Florentiamyidae and Zapodidae. These taxa were correlated with rodents from other North American faunas to establish the age of the Rodent Hill Locality. <p>The species Haplomys cf. H. liolophus, Dakotallomys cf. D. pelycomyoides, Kirkomys milleri, Proheteromys nebraskensis, Agnotocastor cf. A. praetereadens, and possibly Cedromus cf. C. wilsoni support the Whitneyan age designation of the Rodent Hill Locality. Taxa that are described from Rodent Hill that are better known from earlier-age sites include Heliscomys vetus and H. hatcheri, Ecclesimus sp. and Oligotheriomys sp. Taxa that are younger than Whitneyan but have been recovered at Rodent Hill include Parallomys sp., Plesiosminthus sp., Protospermophilus sp., and Nototamias sp. Two new species in the genus Sciurion, and one new species in the genus Pseudallomys are described, and a new species of Heliscomys is identified but not formally named. <p>The rodents from the Rodent Hill Locality support the Whitneyan age assignment of the site. This is based on the presence of Whitneyan taxa, and the in situ co-occurrence of older and younger taxa within the site.

The Rodent Hill Locality is a fossil-bearing site that is part of the Cypress Hills Formation, and is located roughly 15 km northwest of the town of Eastend, Saskatchewan. A number of fossil mammal and other vertebrate taxa are present at Rodent Hill; the primary objective of this project was to identify the fossil rodents of the families Sciuridae, Aplodontidae, Castoridae, Heliscomyidae, Heteromyidae, Florentiamyidae and Zapodidae. These taxa were correlated with rodents from other North American faunas to establish the age of the Rodent Hill Locality. <p>The species Haplomys cf. H. liolophus, Dakotallomys cf. D. pelycomyoides, Kirkomys milleri, Proheteromys nebraskensis, Agnotocastor cf. A. praetereadens, and possibly Cedromus cf. C. wilsoni support the Whitneyan age designation of the Rodent Hill Locality. Taxa that are described from Rodent Hill that are better known from earlier-age sites include Heliscomys vetus and H. hatcheri, Ecclesimus sp. and Oligotheriomys sp. Taxa that are younger than Whitneyan but have been recovered at Rodent Hill include Parallomys sp., Plesiosminthus sp., Protospermophilus sp., and Nototamias sp. Two new species in the genus Sciurion, and one new species in the genus Pseudallomys are described, and a new species of Heliscomys is identified but not formally named. <p>The rodents from the Rodent Hill Locality support the Whitneyan age assignment of the site. This is based on the presence of Whitneyan taxa, and the in situ co-occurrence of older and younger taxa within the site.

No description available.

The Pantano Formation comprises 1,250 m of alluvial, fluvial, lacustrine, and volcanic rocks deposited in a basin formed in response to regional extension during mid- Tertiary time in southeastern Arizona. During deposition, the locations and composition of sediment source areas varied as contemporaneous uplift occurred adjacent to the basin. The lower half of the formation was deposited as alluvial fans that prograded northward, westward, and southward; the upper half was deposited during southwestward retreat of alluvial fan deposition and the onset of lacustrine deposition. An andesite flow separates the two depositional regimes. Radiometric dates of 24.4 ± 2.6 m.y. B.P. for the andesite and 36.7 ± 1.1 m.y. B.P. for a rhyolitic tuff disconformably underlying the formation indicate that deposition occurred during Oligocene to early Miocene time. Proper stratigraphic sequencing and description, paleocurrent analysis, and gravel provenance study aided in understanding the depositional history of the formation.