https://2dgf.dk/cropped-dgf-logo-512px-png/2016-02-16T20:06:58Zhttps://2dgf.dk/wp-content/uploads/2016/02/cropped-dgf-logo-512px.pngcropped-dgf-logo-512px.pnghttps://2dgf.dk/munkholm-bridge-bay/2016-02-17T15:30:27Zhttps://2dgf.dk/wp-content/uploads/2016/02/Munkholm-Bridge-Bay.jpgMunkholm Bridge Bayhttps://2dgf.dk/pdf-1-600x400/2016-02-18T21:13:39Zhttps://2dgf.dk/wp-content/uploads/2016/02/pdf-1-600x400.pngpdf-1-600x400https://2dgf.dk/foreningen/2017-01-17T07:44:34Zhttps://2dgf.dk/wp-content/uploads/2016/02/2dgf_logo_full.png2dgf_logo_fullhttps://2dgf.dk/mt-sample-background/2016-02-21T15:22:01Zhttps://2dgf.dk/wp-content/uploads/2016/02/mt-sample-background.jpgmt-sample-backgroundhttps://2dgf.dk/publikationer/geologisk-tidsskrift/geologisk-tidsskrift-1/2017-02-24T10:43:04Zhttps://2dgf.dk/wp-content/uploads/2016/02/Geologisk-Tidsskrift-2012.jpgGeologisk-Tidsskrift-2012https://2dgf.dk/publikationer/geologisk-tidsskrift/geologisk-tidsskrift-2013/2017-02-24T10:43:05Zhttps://2dgf.dk/wp-content/uploads/2016/02/Geologisk-Tidsskrift-2013.jpgGeologisk-Tidsskrift-2013https://2dgf.dk/publikationer/geologisk-tidsskrift/geologisk-tidsskrift-2014/2017-02-24T10:43:03Zhttps://2dgf.dk/wp-content/uploads/2016/02/Geologisk-Tidsskrift-2014.jpgGeologisk-Tidsskrift-2014https://2dgf.dk/publikationer/bulletin/bulletin-1/2017-02-24T10:42:59Zhttps://2dgf.dk/wp-content/uploads/2016/02/Volume-62-2014-1.jpgVolume-62-2014-1https://2dgf.dk/nyheder/danmarks-geologipris-2014/2017-03-16T13:51:06Zhttps://2dgf.dk/wp-content/uploads/2016/02/dkpris-2014_kurt_h_kjaer.jpgdkpris-2014_kurt_h_kjaerKurt H. Kjær, Statens Naturhistoriske Museum, modtageren af Danmarks Geologipris 2014.https://2dgf.dk/nyheder/danmarks-geologipris-2014/2017-03-16T13:51:05Zhttps://2dgf.dk/wp-content/uploads/2016/02/dkpris-2014_kurt_h_kjaer_overraekkelse.jpgdkpris-2014_kurt_h_kjaer_overraekkelseAdministrerende direktør Johnny Fredericia fra GEUS overrækker Danmarks Geologipris 2014 til Kurt H. Kjær ved Dansk Geologisk Forenings årsmøde i 2015.https://2dgf.dk/foreningen/legater-medaljer/clements-legat/2016-02-24T12:45:35Zhttps://2dgf.dk/wp-content/uploads/2016/02/Clements-Legat-255x300.jpgClements-Legat-255x300https://2dgf.dk/foreningen/legater-medaljer/2016-03-30T21:08:42Zhttps://2dgf.dk/wp-content/uploads/2016/03/dgf-lagater-ikon.pngdgf-lagater-ikonhttps://2dgf.dk/foreningen/legater-medaljer/2016-03-30T21:08:45Zhttps://2dgf.dk/wp-content/uploads/2016/03/clements-legat-ikon.pngclements-legat-ikonhttps://2dgf.dk/foreningen/legater-medaljer/2016-03-30T21:08:46Zhttps://2dgf.dk/wp-content/uploads/2016/03/stenomedaljer-ikon.pngstenomedaljer-ikonhttps://2dgf.dk/publikationer/geologisk-tidsskrift/geologisk-tidsskrift-2011/2016-05-17T17:49:54Zhttps://2dgf.dk/wp-content/uploads/2016/05/gt2011-forside.jpggt2011-forsidehttps://2dgf.dk/bull-fors/2017-02-24T10:42:56Zhttps://2dgf.dk/wp-content/uploads/2016/05/bull-fors.jpgbull-forshttps://2dgf.dk/foreningen/legater-medaljer/stenomedaljen/2016-05-26T11:40:07Zhttps://2dgf.dk/wp-content/uploads/2016/02/stenoguld.jpgstenoguldhttps://2dgf.dk/foreningen/legater-medaljer/stenomedaljen/2017-03-16T13:51:02Zhttps://2dgf.dk/wp-content/uploads/2016/02/steno98.jpgsteno98https://2dgf.dk/arkiv/aarsskrift/2016-05-26T13:00:11Zhttps://2dgf.dk/wp-content/uploads/2016/05/aarsskrift_forside.jpgaarsskrift_forsidehttps://2dgf.dk/dgf-online-series/swimming-patterns-of-malagasyan-triassic-fishes-and-environment/2016-05-26T13:30:55Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_bartieri-martin1.gifols_bartieri-martin1https://2dgf.dk/dgf-online-series/swimming-patterns-of-malagasyan-triassic-fishes-and-environment/2016-05-26T13:30:56Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_bartieri-martin2.gifols_bartieri-martin2https://2dgf.dk/dgf-online-series/swimming-patterns-of-malagasyan-triassic-fishes-and-environment/2016-05-26T13:30:57Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_bartieri-martin3.gifols_bartieri-martin3https://2dgf.dk/dgf-online-series/swimming-patterns-of-malagasyan-triassic-fishes-and-environment/2016-05-26T13:30:57Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_bartieri-martin4.gifols_bartieri-martin4https://2dgf.dk/dgf-online-series/discovery-of-the-ichthyosaur-ophthalmosaurus-reptilia-in-the-late-jurassic-of-the-boulonnais/2016-05-26T13:35:12Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_bardet2.gifols_bardet2https://2dgf.dk/dgf-online-series/discovery-of-the-ichthyosaur-ophthalmosaurus-reptilia-in-the-late-jurassic-of-the-boulonnais/2016-05-26T13:35:14Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_bardet1.gifols_bardet1https://2dgf.dk/dgf-online-series/the-unfinished-story-of-the-early-tertiary-giant-bird-gastornis/2016-05-26T13:37:51Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_buffetaut2.gifols_buffetaut2https://2dgf.dk/dgf-online-series/the-unfinished-story-of-the-early-tertiary-giant-bird-gastornis/2016-05-26T13:37:52Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_buffetaut1.gifols_buffetaut1https://2dgf.dk/dgf-online-series/argentinean-theropods-first-morphological-analysis-on-isolated-teeth/2016-05-26T13:40:03Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_buscalioni1-e1464270032159.gifols_buscalioni1https://2dgf.dk/dgf-online-series/argentinean-theropods-first-morphological-analysis-on-isolated-teeth/2016-05-26T13:40:04Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_buscalioni2.jpgols_buscalioni2https://2dgf.dk/dgf-online-series/supposed-and-direct-evidence-of-trophic-relationships-within-the-marine-fish-community-from-the-lower-turonian-of-goulmima-morocco/2016-05-26T13:44:13Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_cavin1.gifols_cavin1https://2dgf.dk/dgf-online-series/supposed-and-direct-evidence-of-trophic-relationships-within-the-marine-fish-community-from-the-lower-turonian-of-goulmima-morocco/2016-05-26T13:44:14Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_cavin2.gifols_cavin2https://2dgf.dk/dgf-online-series/a-batrachosauroididae-amphibia-caudata-from-the-late-cretaceous-of-champ-garimond-southern-france/2016-05-26T13:46:27Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_duffaud1.jpgols_duffaud1https://2dgf.dk/dgf-online-series/notes-on-palaeornithology-and-on-a-new-bird-from-the-early-tertiary-north-sea-region/2016-05-26T13:48:05Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_hoch1.jpgols_hoch1https://2dgf.dk/dgf-online-series/notes-on-palaeornithology-and-on-a-new-bird-from-the-early-tertiary-north-sea-region/2016-05-26T13:48:06Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_hoch2.jpgols_hoch2https://2dgf.dk/dgf-online-series/reconstruction-of-the-paleoecology-of-the-metriorhynchidae-crocodylia-thalattosuchia-morphofunctional-analysis-and-histological-data/2016-05-26T13:49:50Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_hua-et-al1.gifols_hua-et-al1https://2dgf.dk/dgf-online-series/reconstruction-of-the-paleoecology-of-the-metriorhynchidae-crocodylia-thalattosuchia-morphofunctional-analysis-and-histological-data/2016-05-26T13:50:18Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_hua-et-al2.gifols_hua-et-al2https://2dgf.dk/dgf-online-series/new-records-of-perching-birds-from-the-latest-paleoceneearliest-eocene-fur-formation-of-denmark/2016-05-26T13:52:51Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_kristoffersen3.gifols_kristoffersen3Fig.3 Specimen FU100, part and counterpart. Abbreviations R.DI-III, right digit 1-3; R.Fe, right femur; R.Sc, right scapula; R.Ti, right tibiotarsus; R.Tm, right tarsometatarsus; U, ulnare. For other abbreviations and signatures see Fig.1 & 2.https://2dgf.dk/dgf-online-series/new-records-of-perching-birds-from-the-latest-paleoceneearliest-eocene-fur-formation-of-denmark/2016-05-26T13:53:01Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_kristoffersen4.gifols_kristoffersen4 Fig. 1 Fig.1 Specimen Da.k.7, part and counterpart. Abbreviations Fur, furcula; L.Co, left coracoid; L.Fe, left femur; L.Hu, left humerus; L.Ra, left radius; L.Ti, left tibiotarsus; L.Tm, left tarsometatarsus; L.Ul, left ulna; R.Hu, right humerus; R.Ra, right radius; R.Ul, right ulna; S.Ca, sternal carina; I-IV, digit 1-4. Description and comparison Da.k.7 (Fig.1): The fossil specimen consists of humerus, ulna and radius of both wings (the distal ends of left ulna and radius are not preserved), the left coracoid, the furcula, and the sternum is represented by the sternal carina pointing out of the sediment. A complete, articulated left hind limb intersects the radius and ulna of the left wing. Remains of the ungual hornsheaths of the foot and imprints of feathers are preserved. Characters of the coracoid and humerus are distinctive and indicate affinity with the Apodiformes. The prominent and ventrally directed ventral tubercle, the rounded outline of the pectoral crest and broad proximal and distal articulating ends in the humerus, are reminiscent of Apus. The skeletal elements of Da.k.7 are, however much less specialized than in the true swift genus Apus, and more similar to the tree swifts, Hemiprocnidae, and some fossil genera of Apodiformes. Hemiprocnidae, differs from the Apodidae, particular in the wing elements, e.g. by a less specialized humerus, with a longer and more slender shaft and the M. extensor metacarpi radialis and M. tensor propatagialis brevis processes positioned on the lower half of the humerus. Also the elongation of the hand elements is less pronounced. Characters such as the sternal projection of the coracoid, the size and shape of the ventral tubercle, the outline of the bicipital and pectoral crest, the size, depth, position and shape of the brachial fossa, the position and size of the condyles of the humerus together with the size and proportions strongly suggests that Da.k.7 belong to the species Eocypselus vincenti Harrison 1984, known from the Lower Eocene London Clay. The M. tensor propatagialis brevis and the M. extensor metacarpi radialis tubercles cannot be demonstrated in Da.k.7. This might be due to breakage or partly covering by sediment of the dorsal face of the humerus in the distal end, especially if the tubercles are as weakly developed as in Eocypselus. The hind limb of Da.k.7 differ from Apus, in having a very prominent cnemial crest which serves as the attachment for the flexor muscles and a strong anisodactyle foot, with a long backwards pointing hallux, positioned at the same level as the other three digits and the strongly curved unguals with large flexor tubercles are typical of perching birds. The true swifts posses a pamprodactyle foot (all four digits pointing forward), however the tree swifts posses a more typical perching foot in concordance with the fossil specimen. Fig 2 Fig.2 Specimen Da.k.22, part and counterpart. Abbreviations Cos, costae; R, radiale; R.Cm, right carpometacarpus; R.Co, right coracoid; St, sternum R.DIII, right digit 3; R.DII, right digit 2; DII-III, digit 2-3; U, ulnare. For other abbreviations and signatures see Fig.1. Da.k.22 (Fig.2): This fossil specimen consists of a complete, articulated right wing skeleton, the left humerus, the sternum and the proximal parts of both coracoids seen in dorsal view. It exhibits a mixture of characters recognizable in the avian families Alcedinidae, Meropidae, Trogonidae and the Archaeotrogonidae, strongly indicating affinity with the Coraciiformes. The strong medial position of the sternal facet in the coracoid is similar to both the Alcedinidae and the Archaeotrogonidae. In the sternum, the characteristic external spine is similar to the Trogonidae, whereas the thick cranial pilae are more similar to the Alcedinidae and Meropidae. The characters of the humerus, with the rather long and medially positioned humeral head and the almost pointed appearance of the dorsal condyle, show the closest similarity to the Trogonidae and Archaeotrogonidae. The projection in the proximal part of the radius resembles that of the Meropidae and to some extent Trogonidae. Separate characters of the carpometacarpus can be recognized in all of the Coraciiform families. In digit II, the elaboration of the cranial pila and the biconcavity and the shape of phalanx II are reminiscent of the Alcedinidae. The concordance in preserved elements in Da.k.22 and the Archaeotrogons are limited, however, in the few similarly preserved elements a very good agreement in characters can be seen (Fig. 4). The most distinct difference between Da.k.22 and the Archaeotrogons is the actual size, where the Archaeotrogons are two to two and a half time larger than Da.k.22. A new species and possibly even a new genus should be erected for a position of Da.k.22 in this family. Any elements associated with the hind limb has in this fossil specimen not been preserved. The proportions of the preserved skeletal elements and the possible allocation with the Coraciiformes, however, suggests that this was a perching bird. Fig 3 Fig.3 Specimen FU100, part and counterpart. Abbreviations R.DI-III, right digit 1-3; R.Fe, right femur; R.Sc, right scapula; R.Ti, right tibiotarsus; R.Tm, right tarsometatarsus; U, ulnare. For other abbreviations and signatures see Fig.1 & 2. FU100 (Fig.3): This fossil specimen consists of a complete, articulated left wing skeleton, the proximal end of the right humerus, a large part of the shoulder girdle, including the sternum, the right coracoid, the right scapula and fragments of the furcula. The right hind limb is represented by a tibiotarsus and a broken tarsometatarsus, upon which the radius and ulna of the right wing are superimposed. Imprints of feathers, including a flight feathers, are visible. The combination of a proximal, rectangular pectoral crest, a caudal position of the humeral head and the high and prominent external condyle of the humerus and prominent craniolateral processes, slender and relatively long lateral processes and a high external spine in the sternum indicate a close relationship of FU100 with Bucerotiformes and the Passeriformes. A ventral torsion of metacarpal I, craniocaudally flattened metacarpal III, a deep carpal fovea and a narrow carpal trochlea, further support the hypothesis of a close relationship between FU100, Passeriformes and Bucerotiformes. However, the character mosaic and in many bones less specialized features of FU100 prevent it from being classified with either of these two orders. Differences in the elaboration of the sternal rostrum is noticeable between FU100 and species from the latter two orders. The internal spine present in the hoopoe is not demonstrable in FU100, nor is the external spine in FU100 dorsally bifurcated as seen in the majority of passerine birds. However, an ancestral position of FU100 to the Bucerotiformes and Passerifomes would be possible. The elaboration of the procoracoid process and the external spine in FU100 is less specialized than in both the hoopoe and the passerines. Phylogenetically, a continuing growth in height of the procoracoid process, from the state seen in FU100, could result in a fusion with the acrocoracoid process, as seen in the Bucerotiformes. In the passerine lineage the coracoid could have developed, from the state seen in FU100, towards a more reversed condition, with a less pronounced procoracoid process, as seen e.g. in the tyrants, to the slender and delicate coracoid of e.g. the robin, which has a nearly completely reduced procoracoid process. Similar series of transformation could be imagined for characters of the sternum, with a deepening of the sternal incisions, a cranial direction of the craniolateral processes and a bifurcation of the external spine in the passerine lineage and in the Bucerotiform lineage the development of an internal spine. The hind limb of FU100 show, as Da.k.7, features typical of perching birds, with a large cnemial crest and the metatarsal I at the same level as the distal end of the remaining metatarsals. Also a single disarticulated, strongly curved ungual is observable. Fig. 4 Fig.4 A simplified model showing the supposed evolution and interrelationship of the “higher” landbirds.https://2dgf.dk/dgf-online-series/new-records-of-perching-birds-from-the-latest-paleoceneearliest-eocene-fur-formation-of-denmark/2016-05-26T13:52:40Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_kristoffersen1.gifols_kristoffersen1Fig.1 Specimen Da.k.7, part and counterpart. Abbreviations Fur, furcula; L.Co, left coracoid; L.Fe, left femur; L.Hu, left humerus; L.Ra, left radius; L.Ti, left tibiotarsus; L.Tm, left tarsometatarsus; L.Ul, left ulna; R.Hu, right humerus; R.Ra, right radius; R.Ul, right ulna; S.Ca, sternal carina; I-IV, digit 1-4.https://2dgf.dk/dgf-online-series/new-records-of-perching-birds-from-the-latest-paleoceneearliest-eocene-fur-formation-of-denmark/2016-05-26T13:52:47Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_kristoffersen2.gifols_kristoffersen2Fig.2 Specimen Da.k.22, part and counterpart. Abbreviations Cos, costae; R, radiale; R.Cm, right carpometacarpus; R.Co, right coracoid; St, sternum R.DIII, right digit 3; R.DII, right digit 2; DII-III, digit 2-3; U, ulnare. For other abbreviations and signatures see Fig.1.https://2dgf.dk/dgf-online-series/a-titanosaurid-megatracksite-from-the-maastrichtian-of-catalonia-spain/2016-05-26T13:57:04Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_loeuff1.gifols_loeuff1Fig.1: Location of the Fumanya tracksite (square)https://2dgf.dk/dgf-online-series/a-titanosaurid-megatracksite-from-the-maastrichtian-of-catalonia-spain/2016-05-26T13:57:09Zhttps://2dgf.dk/wp-content/uploads/2016/05/ols_loeuff2.gifols_loeuff2Fig. 2 : Map of the northern part of the main slab (scale bar:1 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