574 research outputs found
Dipoides Jaeger 1835
No full textGenus Dipoides Jäger, 1835 Not Dipoides Schlosser, 1902, following Hugueney (1999).Published as part of García-Alix, Antonio, Minwer-Barakat, Raef, Martín-Suárez, Elvira & Freudenthal, Matthijs, 2007, The southernmost record of fossil Castoridae (Mammalia, Rodentia) in Europe, pp. 435-440 in Geodiversitas 29 (3) on page 436, DOI: 10.5281/zenodo.465103
Biostratigraphy and paleoecology of the Neogene micromammalian faunas from the Calatayud-Teruel Basin (Spain) /
No full textIncludes bibliographical references.Synopsis of the Dutch-Spanish collaboration program in the Neogene of the Calatayud-Teruel Basin, 1976-1986 / R. Daams and M. Freudenthal -- Rodents and lagomorphs from a lower Vallesian fissure filling near Molina de Aragon (Prov. de Guadalajara Spain) / J.I. Lacomba Andueza -- Megacricetodon (Cricetidae) from the Aragonian and the lower Vallesian of the Calatayud-Teruel Basin / R. Daams and M. Freudenthal -- Democricetodon, Fahlbuschia, Pseudofahlbuschia nov. gen. and Renzimys from the Aragonian and the lower Vallesian of the Calatayud-Teruel Basin / M. Freudenthal and R. Daams -- Insectivora from the Upper Aragonian and the lower Vallesian of the Calatauid-Teruel Basin / F. de Jong -- Ecostratigraphy of micromammal faunas from the Neogene of the Calatayud-Teruel Basin / R. Daams, M. Freudenthal and A.J. van der Meulen
FIG. 2 in The southernmost record of fossil Castoridae (Mammalia, Rodentia) in Europe
No full textFIG. 2. — Dipoides problematicus (Schlosser, 1902) from the Mio-Pliocene boundary of Granada Basin: A, lower incisor (PUR-23 175); B, left p4-m2 (PUR-23 174); C, D4? (PUR-23 181); D, left P4 (CLC-3B 83); E, right M1-2 (DHS-16 212); F, Left M3 (DHS-16 213). Scale bar: 1 mm.Published as part of García-Alix, Antonio, Minwer-Barakat, Raef, Martín-Suárez, Elvira & Freudenthal, Matthijs, 2007, The southernmost record of fossil Castoridae (Mammalia, Rodentia) in Europe, pp. 435-440 in Geodiversitas 29 (3) on page 438, DOI: 10.5281/zenodo.465103
FIG. 3 in Hypsodont Myomiminae (Gliridae, Rodentia) from five new localities in the Lower Miocene Tudela Formation (Bardenas Reales, Ebro Basin, Spain) and their bearing on the age of the Agenian-Ramblian boundary
No full textFIG. 3. — Distribution chart of the Myomiminae species studied in this paper and in Daams (1990). The succession of the localities from Daams (1990) is, though in stratigraphical order, not calibrated.Published as part of <i>Ruiz-Sánchez, Francisco J., Murelaga, Xabier, Larrasoaña, Juan C., Freudenthal, Matthijs & Garcés, Miguel, 2012, Hypsodont Myomiminae (Gliridae, Rodentia) from five new localities in the Lower Miocene Tudela Formation (Bardenas Reales, Ebro Basin, Spain) and their bearing on the age of the Agenian-Ramblian boundary, pp. 645-663 in Geodiversitas 34 (3)</i> on page 651, DOI: 10.5252/g2012n3a10, <a href="http://zenodo.org/record/5375769">http://zenodo.org/record/5375769</a>
Societal need for multifunctional flood defenses: Introduction
No full textProf.dr.ir. Matthijs Kok is Professor of Flood Risk at the Faculty of Civil Engineering and Geosciences at TU Delft; he was Program leader of the ‘Integral and Sustainable Design of Multifunctional Flood Defenses’ research program, funded by the Dutch Science and Technology Foundation STW. Presently, he is Program leader of the STW-Perspectief research program ‘All RISK’, which will study the implementation of new risk standards in the Dutch national flood protection program (2017-2022). Hydraulic Structures and Flood Ris
The Aragonian type area revisited; comments on paleontology and stratigraphy
No full textIn a recent study of van der Meulen and coauthors, the fossil rodents Fahlbuschia, Pseudofahlbuschia and Renzimys from the Aragonian type area (Calatayud Basin, Spain) were synonimized with Democricetodon. On the basis of the relative chronology provided by Daams and coauthors in an earlier study, these authors construed two evolutionary lineages, distinguished by size. One of these lineages contains Fahlbuschia koenigswaldi (Freudenthal, 1963) and the other one Democricetodon moralesi van der Meulen et al., 2004 but, in view of their great similarity, we consider D. moralesi to be a synonym of F. koenigswaldi. The relative stratigraphic position of some fossil mammal localities is difficult to establish in the Aragonian type area because it is affected by folds and faults. Early studies of Daams and Freudenthal subdivided the local zone D into D1, D2, D3 and gave a scheme of the stratigraphy in which the fossiliferous locality Valdemoros 1A is considered to be older than Valdemoros 3B. But Daams and coauthors came to the opposite interpretation in a later study, and divided zone D in Da, Db, Dc, Dd. But, new field data presented here enforce the original interpretation in which Valdemoros 1A is older than Valdemoros 3B. This leads to the conclusion that the division of local zone D into Da to Dd has to be discarded, and substituted by the formerly proposed zonation D1-D3
The Marine and continental Upper Miocene of Crevillente (Alicante, Spain). The Cricetidae (Mammalia, Rodentia) from the Late Miocene of Crevillente (prov. Alicante, Spain). Revision of the genus Castillomys (Muridae, Rodentia).
No full textThe Marine and continental Upper Miocene of Crevillente (Alicante, Spain) /M. Freudenthal ... [et al.]The Cricetidae (Mammalia, Rodentia) from the Late Miocene of Crevillente (prov. Alicante, Spain) / M. Freudenthal, J.I. Lacomba, E. Martin Suárez.Revision of the genus Castillomys (Muridae, Rodentia) / E. Martin Suárez & P. Mein.Cover title.Includes bibliographical references
The Aragonian type area revisited; comments on paleontology and stratigraphy
No full textIn a recent study of van der Meulen and coauthors, the fossil rodents Fahlbuschia, Pseudofahlbuschia and Renzimys from the Aragonian type area (Calatayud Basin, Spain) were synonimized with Democricetodon. On the basis of the relative chronology provided by Daams and coauthors in an earlier study, these authors construed two evolutionary lineages, distinguished by size. One of these lineages contains Fahlbuschia koenigswaldi (Freudenthal, 1963) and the other one Democricetodon moralesi van der Meulen et al., 2004 but, in view of their great similarity, we consider D. moralesi to be a synonym of F. koenigswaldi. The relative stratigraphic position of some fossil mammal localities is difficult to establish in the Aragonian type area because it is affected by folds and faults. Early studies of Daams and Freudenthal subdivided the local zone D into D1, D2, D3 and gave a scheme of the stratigraphy in which the fossiliferous locality Valdemoros 1A is considered to be older than Valdemoros 3B. But Daams and coauthors came to the opposite interpretation in a later study, and divided zone D in Da, Db, Dc, Dd. But, new field data presented here enforce the original interpretation in which Valdemoros 1A is older than Valdemoros 3B. This leads to the conclusion that the division of local zone D into Da to Dd has to be discarded, and substituted by the formerly proposed zonation D1-D3
Armantomys jasperi Daams 1990
No full textArmantomys cf. jasperi Daams, 1990 (Fig. 4N) HOLOTYPE. — COR 70, left M2 (in Daams 1990: pl. 2; fig. 17). TYPE LOCALITY. — Córcoles, Loranca Basin, Spain. LOCALITY AND AGE. — Cuesta Agujeros 4 (CA 4), Province of Navarre, Spain. Ramblian (Local zone A, MN 3). MATERIAL AND MEASUREMENTS. — CA 4-1/27, incomplete right m2. DESCRIPTION m2 Anterolophid long and separated from the protoconid by a narrow and deep furrow. Near the metaconid, the anterolophid is partially interrupted, thus forming a short posterior spur. Metalophid high connected to the metaconid. The metalophid is continuous with a short fold directed towards the anterolophid, but not connected to that ridge. Centrolophid absent. REMARKS The presence of a short longitudinal spur on the posterior wall of the anterolophid is described in the m2 of A. jasperi from its type locality, Córcoles (Daams 1990). This morphology has not been mentioned in other populations of medium-sized Armantomys species. Therefore, the presence of a short spur on the posterior wall of the anterolophid and the width of the specimen indicate that it belongs to A. jasperi. Nevertheless, the scarcity of material and its fragmentary state do not allow a certain assignment.Published as part of Ruiz-Sánchez, Francisco J., Murelaga, Xabier, Larrasoaña, Juan C., Freudenthal, Matthijs & Garcés, Miguel, 2012, Hypsodont Myomiminae (Gliridae, Rodentia) from five new localities in the Lower Miocene Tudela Formation (Bardenas Reales, Ebro Basin, Spain) and their bearing on the age of the Agenian-Ramblian boundary, pp. 645-663 in Geodiversitas 34 (3) on pages 656-657, DOI: 10.5252/g2012n3a10, http://zenodo.org/record/537576
Correction to: CT angiography vs echocardiography for detection of cardiac thrombi in ischemic stroke: a systematic review and meta-analysis (Journal of Neurology, (2020), 267, 6, (1793-1801), 10.1007/s00415-020-09766-8)
No full textThe original version of this article unfortunately contained a mistake. In the author list, the first and last names of two authors, S. Matthijs Boekholdt and R. Nils Planken, were tagged incorrectly. Therefore, author names are abbreviated wrongly in Springerlink. The first and last names should be as follows: First name: S. Matthijs Last name: Boekholdt First name: R. Nils Last name: Planken
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