P. Louis and J. Sudre. 1975. Nouvelles donnees sur les primates de l'Eocene superieur europeen. Colloque international CNRS, Problemes actuels de paleontologie - evolution des vertebres (218)805-828
W. H. Hudleston. 1902. Creechbarrow: An Esay in Purbeck Geology. Proceedings of the Dorset Natural History Museum and Antiquarian Field Club 23:146-190

Creechbarrow Hill Where: England, United Kingdom (50.7° N, 2.1° W: paleocoordinates 48.6° N, 6.0° W) When: Creechbarrow Limestone Formation, Bartonian (40.4 - 37.2 Ma) • This is the only known outcrop of the Creechbarrow Limestone, ranges in thickness from 0-16 m and lies above unnamed sands and clays Environment/lithology: marine; oncoidal, shelly/skeletal, yellow, sandy marl and intraclastic, shelly/skeletal, yellow, silty, sandy, calcareous marl • in general it's a buff marl containing variable sized limestone clasts, the limestone (sensu stricto) is a cream coloured, mottled with buff, soft to hard, massive micritic limestone with drusy sparite, scattered angular to subangular quartz grains up to 1mm in diameter, oncoliths often containing [molluscs and vertebrate remains]. Hard limestone in recent excavations was mainly encountered in the basal rubbly soid layer (A). •buff marl: a buff calcareous silty clay with abundant angular to subangular quartz grains up to 1 m m in diameter and containing limestone clasts. It also contains oncoliths often containing [mollusc] and vertebrate remains and derived silicified Cretacous bryozoans. Size classes: macrofossils, mesofossils Preservation: cast, trace Primary reference: YUk_Denman MGjn5lHY */ var markerArray = []; var marker = []; var infowindowArray = []; function setMarkers(map, locations) { var image = new google.maps.MarkerImage('/design/pin_green.png', new google.maps.Size(30, 31), new google.maps.Point(0,0), new google.maps.Point(0, 30)); var shadow = new google.maps.MarkerImage('/design/pin_shadow.png', new google.maps.Size(37,11), new google.maps.Point(0,0), new google.maps.Point(1,3)); var shape = { coord: [21,0,31,8,18,16,15,26,5,17], type: 'poly' }; for (var i = 0; i < locations.length; i++) { var species = locations[i]; var myLatLng = new google.maps.LatLng(species[1], species[2]); marker[i] = new google.maps.Marker({ position: myLatLng, map: map, shadow: shadow, icon: image, shape: shape, title: species[0], zIndex: species[3] }); marker[i].myInhalt= species[4]; marker[i].setMap ( map ); google.maps.event.addListener( marker[i] , 'click', function() { myFenster ( this); }); } var infowindow = new google.maps.InfoWindow(); function myFenster (myMarker) { infowindow.close(); infowindow.setPosition(myMarker.getPosition()); infowindow.setContent(myMarker.myInhalt); infowindow.open(map); } } Pseudoloris crusafonti

 

Pseudoloris crusafonti

Zeitraum: spates Eozän bis frühes Oligozän
Verbreitung: Europa
Gewicht:  
Art: P. crusafonti
Systematik
ein aus
 

Pseudoloris crusafonti ist der Name eines ausgestorbenen Primat aus der Familie Omomyidae (Unterfamilie Microchoerinae), der im Eozän in Europa verbreitet war.

Das Typusexemplar mit der Bezeichnung Gri. 382 ist ein rechter oberer Molar (M2). Der Fund stammt aus der Calcaire de Saint-Ouen Formation und ist zwischen 40,4 und 37,2 Millionen Jahre alt.

Basierend auf der Morphologie der Funde geht man davon aus, dass Pseudoloris crusafonti ein baumlebender Insektenfresser war.

P. Louis and J. Sudre. 1975. Nouvelles donnees sur les primates de l'Eocene superieur europeen. Colloque international CNRS, Problemes actuels de paleontologie - evolution des vertebres (218)805-828

W. H. Hudleston. 1902. Creechbarrow: An Esay in Purbeck Geology. Proceedings of the Dorset Natural History Museum and Antiquarian Field Club 23:146-190

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