1830–1840s: Friedrich von Hagenow – Maastrichtian of the Isle of Rügen

Karl Friedrich von Hagenow (1797–1865; Fig. 2A) was born into an aristocratic family and grew up in Western Pomerania (Beyrich, Reference Beyrich1866; Pyl, Reference Pyl1866). At an early age von Hagenow's tutor (and later stepfather), Gustav Salomon Tillberg (1777–1859), aroused his interest in natural sciences and arranged that he could attend the University of Greifswald in 1809, when the gifted boy was only 12 years old. His principal studies included mathematics, mechanics and ornithology. Von Hagenow had a lifelong vivid interest in prehistory and he carried out the topographical surveying of Neu-Vorpommern (formerly Swedish Pomerania) between 1825 and 1828, for which in 1830 he obtained an honorary doctoral degree from the University of Greifswald. In 1832 von Hagenow purchased a grant licence for the exclusive chalk exploitation on the peninsula of Jasmund, Isle of Rügen (von Hagenow, Reference von Hagenow1838). In the same year he opened a chalk factory in his place of residence at Greifswald with machines and equipment that he personally designed (Boll, Reference Boll1865; Habetha, Reference Habetha1939; J. Ansorge & M. Reich unpublished data). As an additional gain of the precipitate chalk production von Hagenow amassed one of the largest collections of chalk fossil of his time, which contained around 100,000 specimens by the end of the 1830s (von Hagenow, Reference von Hagenow1839).

Fig. 2.

(A) Friedrich von Hagenow (GG archives, modified). (B) Drawing of a mosasaur tooth crown from Blandow on the Isle of Rügen by von Hagenow (unpublished manuscript, UBG).

From this von Hagenow’s most eminent opus resulted, the Monographie der Rügen’schen Kreide-Versteinerungen (Monograph on the Cretaceous fossils from Rügen) of which three volumes were published, dealing with invertebrate fossils (von Hagenow, Reference von Hagenow1839, Reference von Hagenow1840, Reference von Hagenow1842). A fourth volume that should have included the arthropod and vertebrate fossils was never completed due to the delayed return (after 5 years) of fish material sent on loan to Louis Agassiz (Paris and Neuchâtel) and von Hagenow's deteriorating eyesight after 1846. However, some illustrations had been finished, which are preserved as manuscripts in the Greifswald University library (Reich & Frenzel, Reference Reich and Frenzel2002). Among them is the drawing of a well-preserved crown of a marginal mosasaur tooth from the Lower Maastrichtian chalk of Blandow on the Isle of Rügen (Western Pomerania, northeastern Germany) that was prepared on the basis of material von Hagenow collected in the 1830s (see also Reich & Frenzel, Reference Reich and Frenzel2002: pl. 2, fig. 4). This drawing is the earliest unambiguous document of a mosasaur fossil found in Germany. Later authors, especially Deecke (Reference Deecke1895, Reference Deecke1907), commented briefly on the existence of mosasaur tooth crowns in the collection of von Hagenow. However, most of his material from the chalk of Rügen was destroyed at Stettin (now Szczecin, Poland) during World War II (Voigt, Reference Voigt1959; Steinich, Reference Steinich1965; pers. comm. W. Filipowiak, 1997), and only a few specimens (long-term loans before 1945) survived at Greifswald University, including a single fragment of a mosasaur tooth crown (Reich & Frenzel, Reference Reich and Frenzel2002), which is not identical to the splendid specimen figured by von Hagenow (in his estate). Recently, Jagt et al. (Reference Jagt, Motchurova-Dekova, Ivanov, Cappetta and Schulp2006) proposed that von Hagenow's specimen might represent another individual of the tylosaurine Hainosaurus ‘sp. 2’, which had been described earlier from the Lower Maastrichtian of Poland (Jagt et al., Reference Jagt, Lindgren, Machalski, Radwański, Schulp and Jagt2005). However, for reasons discussed in Hornung & Reich (Reference Hornung and Reich2014), it seems more probable that it can be referred to a species of Mosasaurus Conybeare in Parkinson, Reference Parkinson1822, most probably to M. hoffmanni Mantell, Reference Mantell1829. This is congruent with the assignment von Hagenow made on his original illustration (Fig. 2B).

Fig. 3.

(A) Hermann von Meyer (from Langer Reference Langer, Goth, Haas and Mai1997, modified). (B) tooth crown referred to Liodon anceps? by Wagner (Reference Wagner1853) found nearby Regensburg. (C) Holotype tooth crowns of Liodon paradoxus found in Ihrlerstein, formerly Neukelheim (from Wagner Reference Wagner1853). Scale bar equals 2 cm.

1853–1856: Hermann von Meyer and Andreas Wagner – Turonian/Cenomanian of the Regensburg area

In 1853 Hermann von Meyer briefly mentioned an incomplete reptilian tooth crown allegedly from the Regensburger Grünsand[stein] (now Regensburg Formation, Turonian/Cenomanian; see Wilmsen et al., Reference Wilmsen, Wood, Niebuhr and Kaplan2009) found by Professor Karl Emil von Schafhäutl (1803–1890) at an uncertain locality in the vicinity of Regensburg (Bavaria, southeast Germany) (von Meyer, Reference von Meyer1853).

Christian Erich Hermann von Meyer (1801–1869; Fig. 3A) was born, grew up and lived for most of his life in Frankfurt am Main (Zittel, Reference Zittel1870). From 1822 to 1827 he studied natural sciences, and geology and mineralogy in particular, at Heidelberg, Munich and Berlin. In 1837 he accepted a position in the financial administration of the German parliament, where he worked for the rest of his career. Perhaps on recommendation of his childhood friend, the well-known chemist Friedrich Wöhler (1800–1882), the University of Göttingen offered him a professorship of Geology and Palaeontology in 1860, which, however, he turned down in order to be able to continue to work independently. Von Meyer carried out all of his voluminous scientific work in his spare time. He did not maintain a significant personal fossil collection, but instead worked on material sent to him by collectors and fellow scientists. Specialising in vertebrates, but with a focus on ‘saurians’, he is today considered the father of vertebrate palaeontology in Germany and one of the most preeminent figures of his days in this field of science. Hermann von Meyer was the co-founder and co-editor of the journal Palaeontographica (founded in 1846) and was a skilful artist who drew all the illustrations for his publications himself (Keller & Storch, Reference Keller, Storch, Keller and Storch2001).

Fig. 4.

(A) cf. Clidastes sp., slab with neural spines (GPIM A.3D2, specimen A) from the Upper Campanian of the Schöppinger Berg. (B) Hanns Bruno Geinitz (GZG archives, modified). Possible squamate vertebra SaK 1748 from the Cenomanian of Dresden in (C) articular and (D) lateral views. Scale bars equal 5 cm (A) and 2 cm (C, D).

Von Meyer named some of the most famous fossil vertebrate taxa, including the first dinosaur found in Germany, the sauropodomorph Plateosaurus engelhardti von Meyer, Reference von Meyer1837, and the first fossil of a Mesozoic bird, the feather of Archaeopteryx lithographica von Meyer, Reference von Meyer1861. In 1832, he also – independently from Richard Owen – recognised that all genera of dinosaurs then known formed a distinct group (von Meyer, Reference von Meyer1832, p. 210), although his proposal to name them ‘Pachypodes’ (von Meyer, Reference von Meyer1845) never caught on. His work and style of thinking was that of a practical observer; it shows few, if any, indications of having been influenced by subjective theories, philosophies or religious beliefs. He observed the occurrences of extinction and gradual changes in the organisms at an early stage of his research (von Meyer, Reference von Meyer1832), although he did not try to elaborate on them in a theoretical way or to unify them in a major hypothesis. Nonetheless he rejected the concept of catastrophism and considered the emergence of new species as a continuous, gradual and natural process (von Meyer, Reference von Meyer1832, Reference von Meyer1852; Hertler, Reference Hertler, Keller and Storch2001; Keller & Storch, Reference Keller, Storch, Keller and Storch2001). In the debate following the publication of Charles Darwin's On the Origin of Species (1859) he remained rather neutral and non-committed. Consequently, he did note the presence of true feathers but also of skeletal differences between Archaeopteryx lithographica and extant birds as a matter of fact, yet did not dwell on their meaning for evolution (Wellnhofer, Reference Wellnhofer, Keller and Storch2001).

His work included occasional references to mosasaurs (von Meyer, Reference von Meyer1832, Reference von Meyer1853, Reference von Meyer1856, Reference von Meyer1860), especially to the material from the Maastricht area. In 1832 he proposed the species name Mosasaurus camperi for all mosasaur material then known from England (UK), Maastricht (the Netherlands) and New Jersey (USA). However, M. camperi is a junior synonym of M. hoffmanni Mantell, Reference Mantell1829 (see Bronn, Reference Bronn1838; Spamer et al., Reference Spamer, Daeschler and Vostreys-Shapiro1995).

Wagner (Reference Wagner1853) formally described the tooth crown that was found by von Schafhäutl (Fig. 3B) and donated by him to the Geognostische Sammlung des Staates Bayern (Geognostic Collection of the State of Bavaria) at Munich.

Johann Andreas Wagner (1797–1861) studied natural sciences, in particular zoology, at Würzburg and Erlangen. At the beginning of his academic career he worked on extant molluscs. In 1832, Wagner was appointed professor in Munich, in charge of the zoological cabinet that also included the palaeontological collection. Besides extensive studies on extant mammals and birds, his work focused on extinct faunas and in particular the fossils found in Bavaria. Wagner was a conservative with a strong faith in Christianity, and a fierce and derisive opponent of the theory of descent as proposed by Darwin in 1859 (von Martius, Reference von Martius1862). He considered this to be scientific fantasy, entirely devoid of evidence. In an ironic twist of historical fate, he was the first to describe scientifically two of the most iconic evidences for evolution which turned up during this time of scientific revolution, although he did not recognise their meaning, nor was even eager to diminish their significance. In the last year before his death, he described a theropod dinosaur from the Upper Jurassic Solnhofen limestones, which he had earlier named Compsognathus longipes Wagner, Reference Wagner1859 and which he considered to be a giant, bipedal lizard (Wagner, Reference Wagner1861a). Shortly afterwards, in a story that is more extensively told by Wellnhofer (Reference Wellnhofer2009), his assistant, Carl Albert Oppel (1831–1865), showed him a sketch of a new ‘reptile with feathers’ that had been found in the same strata and offered for sale by its proprietor. This specimen was sold shortly afterwards to the British Museum in London, where it became known as the London specimen of Archaeopteryx lithographica, a taxon originally based on von Meyer's (Reference von Meyer1861) single feather. Without the opportunity to study the original specimen, Wagner dismissed the transitional nature of the specimen, and the impressions surrounding the bone being evidence of feathers, considering it a ‘reptile with special adornments’, and proposed the name Griphosaurus (‘miracle lizard’) for it (Wagner, Reference Wagner1861b). Near the end of the year of these important discoveries, in December 1861, Wagner died. The fact that Compsognathus longipes was a dinosaur – in fact the most complete one known at the time – and the implications of its similarity with Archaeopteryx lithographica, were shortly after extensively elucidated by Gegenbaur (Reference Gegenbaur1863), Cope (Reference Cope1867) and, most prominently, Huxley (e.g. 1868, 1870).

Wagner (Reference Wagner1853) referred the tooth fragment found by Professor von Schafhäutl to Liodon anceps? Owen, 1841 in Owen (1840–1845) on account of morphological similarities to the teeth of that taxon described and illustrated by Owen (1840–1845). Two other tooth crowns (Figs 3C and D) from Neukelheim (now Ihrlerstein, Bavaria), also supposed to be from the Regensburg Formation, were considered to be a distinct new species by Wagner (Reference Wagner1853), and named Liodon paradoxus. Although these teeth did not closely resemble Owen’s (1840–1845) teeth of L. anceps, Wagner (Reference Wagner1853) supposed that they could be pterygoid teeth of that taxon. The same teeth were further discussed by von Meyer (Reference von Meyer1856). He agreed with Wagner's (Reference Wagner1853) generic assignment, but questioned the taxonomic validity of L. paradoxus since that species had been established on the basis of only minor differences to the other tooth from the Regensburg Greensand that Wagner (Reference Wagner1853) referred to L. anceps?. In all probability, the material was destroyed together with many other specimens from the Munich collection by bombing raids in 1944 (e.g. Nothdurft et al., Reference Nothdurft, Smith, Lamanna, Lacovara, Poole and Smith2002).

Although suffering from loss of material and incomplete original data, today a mosasaur affiliation of von Meyer's and Wagner's material can almost certainly be ruled out. Schlosser (1881, p. 58) listed ‘Liodon anceps und paradoxus Wagner [1853]. […] Taf. III, fig. 6-13’ as ‘Dacosaurus maximus Quenst’ (sic! – the correct taxon name is Dakosaurus maximus (Plieninger, Reference Plieninger1846), see Young et al., Reference Young, Brusatte, de Andrade, Desojo, Beatty, Steel, Fernández, Sakamoto, Ruiz-Omeñaca and Schoch2012) and claimed that the remains of matrix on ‘two’ of the teeth (which apparently belonged to a larger set of specimens than those figured by Wagner (Reference Wagner1853)) from Ihrlerstein (Neukelheim)) indicated that they are Upper Jurassic in age rather than Upper Cretaceous. Fraas (1902, pl. II, figs.: 1, 12–14) figured a partial dentary and a tooth from the Upper Jurassic of Schnaitheim as ‘Dacosaurus paradoxus Wagner em. Fraas’. This material shows close similarity to the now lost teeth figured by Wagner (1853, pl. 3, figs. 9–13), supporting a Upper Jurassic age and an assignment to D. maximus, representing teeth from the rostral part of the jaws (Young et al., Reference Young, Brusatte, de Andrade, Desojo, Beatty, Steel, Fernández, Sakamoto, Ruiz-Omeñaca and Schoch2012).

Fig. 5.

(A) Mosasauridae indet., caudal vertebra from the Upper Campanian of former East Prussia (from Schroeder, Reference Schroeder1885a). (B) Mosasaurus? alseni Stolley, Reference Stolley1892, tooth crown, uppermost Santonian to Lower Campanian of Lägerdorf (from Stolley, Reference Stolley1892). Scale bar equals 3 cm.

The third tooth, first described by von Meyer (Reference von Meyer1853), referred to L. anceps? by Wagner (1853, pl. 3, figs. 6–8), included summarily in D. maximus by Schlosser (Reference Schlosser1881) and Fraas (1902, p. 7), but not by Young et al. (Reference Young, Brusatte, de Andrade, Desojo, Beatty, Steel, Fernández, Sakamoto, Ruiz-Omeñaca and Schoch2012), lacks precise age and locality data, but was assumed by Wagner (1853, p. 21) to have come from the same area and stratum based on its appearance. Its morphology is also consistent with that of the massive, cone-shaped caudad teeth of D. maximus (see Mason, Reference Mason1869; Young et al., Reference Young, Brusatte, de Andrade, Desojo, Beatty, Steel, Fernández, Sakamoto, Ruiz-Omeñaca and Schoch2012). The robust tooth crown, which may be reconstructed to a height of about 60 mm based on the data supplied by Wagner (Reference Wagner1853), would have been unusually large for a Turonian or Cenomanian mosasauroid but fits the dimensions and morphology of D. maximus well.

1858: Wilhelm von der Marck – Campanian Schöppingen

Johann Wilhelm Carl Theodor Matthias von der Marck (1815–1900) was a pharmacist at Hamm in Westphalia. He had a vivid interest in various fields, such as agronomy, botany, chemistry, meteorology, pharmacy, prehistory, geology, mineralogy and palaeontology, and published, between 1845 and 1894, a total of 130 works (Riegraf, 1995). His first palaeontological paper, a short note on petrified wood found near Siegburg, appeared in 1849 (von der Marck, Reference von der Marck1849). Wilhelm von der Marck is well known for his studies on Campanian fishes from Sendenhorst. Fossil reptiles were only considered in his 1858 publication Ueber einige Wirbelthiere, Kruster und Cephalopoden des Westfälischen Kreide (On some vertebrates, crustaceans and cephalopods of the Westphalian Cretaceous, von der Marck, Reference von der Marck1858) and a later popular publication (von der Marck, Reference von der Marck and Landois1892). Von der Marck (1858) summarised the discoveries made at the Schöppinger Berg (near Schöppingen, North Rhine-Westphalia, western Germany) between 1853 and 1857 (these specimens are from the Upper Campanian Coesfeld Formation). He reported that an articulated series of procoelous vertebrae was found around 1853. In the summer of 1857 two more specimens were discovered at the Schöppinger Berg, a fragment of a lower jaw (a dentary with damaged teeth) and a block with four procoelous vertebrae and eight ribs. Furthermore von der Marck (Reference von der Marck1858) mentioned another series of five to six dorsal vertebrae from the collection of Kreisrichter (district judge) Ziegler at Ahaus. Today, the University of Münster houses some mosasaur specimens from the Schöppinger Berg. Among the material from the axial skeleton there is a slab with 11 partially damaged neural spines of dorsal vertebrae and most of one centrum (GPIM A.3D2; see Fig. 4A, here referred to as specimen A). Another specimen (same specimen number GPIM A.3D2; here referred to as specimen B) includes four caudal vertebrae in two slabs (see Sachs, Reference Sachs2000, fig. 4). These specimens are part of the von der Marck Collection, but it is not documented when each was collected. Judging from von der Marck's (Reference von der Marck1858) description as a block with four procoelous vertebrae, about one cubic foot in size, it seems plausible that GPIM A.3D2 (specimen B) is the one found in 1857. Likewise GPIM A.3D2 (specimen A) might be the one found around 1853 but may have suffered some damage since von der Marck’s description. Unfortunately, this cannot be proved since von der Marck (Reference von der Marck1858, Reference von der Marck and Landois1892) did not figure the reptilian specimens. The whereabouts of the vertebrae from the Ziegler Collection are unclear, whereas the dentary fragment went to Teylers Museum in Haarlem (the Netherlands) (von der Marck, Reference von der Marck and Landois1892). Von der Marck asked Hermann von Meyer (see above) to identify the specimens. Meyer believed that the jaw fragment belonged to Mosasaurus gracilis Owen, Reference Owen1851 and the other specimens to Mosasaurus camperi von Meyer, Reference von Meyer1832. Recently Sachs (Reference Sachs2000) and Caldwell & Diedrich (Reference Caldwell, Diedrich, Schulp and Jagt2005) redescribed the available mosasaur material from the Schöppinger Berg. Sachs (Reference Sachs2000) identified the specimens as Mosasauria indet. (not as ?Plioplatecarpus, nor as ?Leiodon sp. as stated by Caldwell & Diedrich, Reference Caldwell, Diedrich, Schulp and Jagt2005), whereas Caldwell & Diedrich (Reference Caldwell, Diedrich, Schulp and Jagt2005) referred to GPIM A.3D2 (specimen A) as cf. Clidastes sp. GPIM A.3D2 (specimen B) was not included in the study of Caldwell & Diedrich (Reference Caldwell, Diedrich, Schulp and Jagt2005); it was assigned to Mosasauria indet. by Sachs (Reference Sachs2000). Neither Sachs (Reference Sachs2000) nor Caldwell & Diedrich (Reference Caldwell, Diedrich, Schulp and Jagt2005) discussed the jaw fragment that went into the collection of the Teylers Museum.

1875: Hanns Bruno Geinitz – Cenomanian of Dresden

Alleged mosasaur material from the Cenomanian of Saxony (eastern Germany) was described in 1875 by Hanns Bruno Geinitz. Geinitz (1814–1900; Fig. 4B) studied natural sciences at the universities of Berlin and Jena, and later rose through the academic and administrative ranks at Dresden. In 1846 he was appointed inspector of the royal mineral collection, in 1850 he was appointed professor at the Königliche Polytechnische Schule (Royal Polytechnical School), and finally, in 1857 became director of the Königliches Mineralogisches und Geologisches Museum (Royal Museum of Mineralogy and Geology) until his retirement in 1894 (Geinitz, Reference Geinitz1900; Grunert & Grunert, Reference Grunert and Grunert2001). His major contributions dealt with a wide range of fossils (e.g. Geinitz Reference Geinitz1846, 1861–1862) and other aspects of geosciences. He extensively worked on local fossil occurrences, whereas his most important contributions to local Cretaceous palaeontology, e.g. Das Quadersandsteingebirge oder Kreidegebirge in Deutschland (The ashlar sandstone stratum or Cretaceous stratum in Germany) and Das Elbthalgebirge (The Elbe Valley stratum), were published in several volumes (Geinitz 1849–1850, 1871–1875, 1872–1875). In the first part of the latter work some fragmentary teeth found in the Upper Cenomanian Döltzschen Formation at Dresden-Plauen and at the Gamighügel in Dresden were described and figured (Geinitz 1871–1875: pl. 65, fig. 45; modern collection numbers SaK 3402 and SaK 7818). Geinitz tentatively referred them to Leiodon anceps? because of a similar morphology to a tooth depicted by Owen (1850, pl. 38, figs. 8, 9). However, the general morphology differs from that of mosasaur teeth (i.e. labiolingually compressed shape and lack of enamel ornamentation) and they may probably be attributed to enchodontid actinopterygians (Kear et al., Reference Kear, Sachs, Ekrt, Hornung, Polcyn and Jacobs2013). Another fragmentary specimen from Dresden-Plauen was described and figured by Geinitz (1871–1875: pl. 66, fig. 1, modern collection number SaK 1748) as the proximal end of a reptilian humerus. It bears a convex articular surface and might be a very fragmentary procoelous vertebral centrum (Figs 4C and D), typical of a squamate (Kear et al., Reference Kear, Sachs, Ekrt, Hornung, Polcyn and Jacobs2013).

1885: Henry Schroeder – Campanian of East Prussia

In 1885 Henry Schroeder published a description of Upper Cretaceous marine reptile remains from the Baltic, including specimens from East and West Prussia and from Sweden (Schroeder, Reference Schroeder1885a). Henry Schroeder (1859–1927) grew up in East Prussia. He was born in Pillau (now Baltisk, Russian Federation) and attended the grammar school at Königsberg (now Kaliningrad, Russian Federation). From 1883 to 1924, Schroeder was Landesgeologe (state geologist) at the Preussische Geologische Landesanstalt (Prussian Geological Survey) at Berlin. In 1920 he became director of the collections department, which included the stratigraphical, geological, palaeozoological and palaeobotanical collections and the library of the Geological State Museum of the survey (Schmierer, Reference Schmierer1928). One of his major tasks was to reorder the systematic palaeontological collection stratigraphically. Schroeder started his early career with contributions on local geology and stratigraphy (e.g. Schroeder, Reference Schroeder1882); his later studies focused to a large degree on fossil vertebrates and in particular on Cenozoic mammals. Schroeder's work on Mesozoic tetrapods included nothosaurs and temnospondyls from the Triassic and marine crocodiles from the Lower Cretaceous.

Among the East Prussian material Schroeder (Reference Schroeder1885a,Reference Schroederb) described, only a single isolated, partly damaged, strongly procoelous vertebra could be assigned to a mosasaur (see Schroeder, Reference Schroeder1885a, pl. 17, fig. 1; see Fig. 5A here); all other specimens belonged to plesiosaurs. The mosasaur vertebra represents an intermediate caudal centrum (sensu Russell, Reference Russell1967, showing haemapophyses as well as the bases of caudal ribs) that was found in an local erratic boulder (from the ‘Mucronaten-Senon’ = lower Upper Campanian) in a sand and gravel pit east of Lauth near Königsberg. Upper Campanian strata are widespread in the subsurface of former East Prussia (e.g. Gagel & Kaunhowen, Reference Gagel and Kaunhowen1900; Spulski, Reference Spulski and Tornquist1910) and therefore local glacial erratic boulders (Geschiebe) of the same age are also very common (e.g. Schroeder, Reference Schroeder1882). The specimen was kept in the Ostpreußisches Provinzial-Museum (East Prussian Provincial Museum) at Königsberg; its current whereabouts are unknown. Schroeder (Reference Schroeder1885a,Reference Schroederb) referred the specimen to Mosasaurus camperi (= M. hoffmanni), on account of a similarity to a vertebra figured by Cuvier (Reference Cuvier, Dufour and d’Ocagne1824). Although he correctly described the vertebra as a caudal, he erroneously interpreted the preserved ventral (haemapophyseal) and lateral (caudal rib) bases of processes as parapophyses and diapophyses, respectively. Judging from Schroeder's (1885a, pl. 17, fig. 1) illustration, the vertebra apparently suffered crushing, which resulted in the asymmetric right lateral exposure of the opposite left base of the neurapophysis and a ventral displacement of the right bases of the neurapophysis and caudal rib. It lacks diagnostic characters and cannot be further identified at the generic level.

Fig. 6.

(A) Josef Felix Pompeckj (GZG archives, modified). (B) Cranial remains of a mosasaur from the Upper Campanian of Haldem (GZG.V.10024), referred to as Mosasaurus cf. mosasauroides by Pompeckj (Reference Pompeckj1910). (C) Painting of Mosasaurus with sharks, inspired in part by the Haldem specimen, by Franz Roubal under instructions of Othenio Abel (1937, oil on canvass, ca. 230 × 105 cm, GZG.A.5440).

1892: Ernst Stolley – Campanian of Lägerdorf

In 1889 two reptilian teeth were found at the Alsen chalk pit (uppermost Santonian to Lower Campanian) near Lägerdorf (Holstein, northern Germany). They stirred some local interest (including press reports) and were finally donated by the pit owner, Mr Alsen, to the geological collection of the Christian-Albrechts University at Kiel. Ernst Stolley included them in his doctoral thesis Die Kreide Schleswig-Holsteins (The Cretaceous of Schleswig-Holstein), which was completed in 1891 at Munich University and published the following year (Stolley, Reference Stolley1892).

Ernst Stolley (1869–1944) studied geology and palaeontology at Kiel and Munich, and was later a professor of geology and palaeontology at the Technische Universität (Technical University) at Braunschweig (Brunswick) from 1901 to 1935. He was one of the most eminent experts on Cretaceous strata in northern Germany and vicinity. His palaeontological work mostly focused on belemnites and stratigraphy, but he also covered a wide range of other topics, including Triassic fishes. Most of his collections and scientific estate was destroyed within months of his death, when the Braunschweig University was hit during a bombing raid in 1944 (Dorn, Reference Dorn1944), although the mosasaur tooth crowns survived at Kiel University.

Stolley (Reference Stolley1892) gave an extensive description of the teeth and figured one of them accurately (Fig. 5B; Hornung & Reich, Reference Hornung and Reich2014). Having noted differences to the teeth of Mosasaurus hoffmanni, he established a new species which he reluctantly referred to the genus as M.? alseni. Despite the good description, this taxon seems to have been forgotten in the following decades. A reassessment of the specimens (Hornung & Reich, Reference Hornung and Reich2014) has resulted in a reassignment to Tylosaurus sp., morphologically close to Tylosaurus ivoensis (Persson, Reference Persson1963), from the Lower Campanian of southern Sweden (Lindgren & Siverson, Reference Lindgren and Siverson2002). However, based on the fact that congruence in the marginal tooth morphology of tylosaurines may not be sufficient to diagnose species reliably (Lindgren & Siverson, Reference Lindgren and Siverson2002) and in view of the small sample, Mosasaurus? alseni is considered a nomen dubium instead of an unambiguous senior synonym of T. ivoensis (for more details, see Hornung & Reich, Reference Hornung and Reich2014).

1902: August Wollemann – Campanian of Lüneburg

Ernst August Wollemann (1862–1920) was a geologist and a teacher. After studying natural sciences and finishing his doctoral studies at Würzburg University in 1887, he returned to his home region in Lower Saxony and became a teacher in Braunschweig. August Wollemann was an active member of the Verein für Naturwissenschaft in Braunschweig (Braunschweig Association for Natural Sciences) as well as a correspondent of the Prussian Geological Survey. His geological studies were focused mainly regionally with publications on Cretaceous invertebrates (primarily molluscs, e.g. Wollemann, Reference Wollemann1900, Reference Wollemann1906, Reference Wollemann1908). Besides this, he also wrote school geography books (e.g. Wollemann, Reference Wollemann1905, Reference Wollemann1910). In 1902, Wollemann published a descriptive overview of the Cretaceous fauna of Lüneburg (Lower Saxony, northern Germany) in which he briefly mentioned two incomplete, isolated reptilian teeth from the Belemnitella mucronata cephalopod zone (lower Upper Campanian), which he tentatively referred to Mosasaurus. Unfortunately, Wollemann (1902) did not describe nor illustrate the specimens so his assignment cannot be verified. He did not specify the collection in which the specimens were housed either. They are not present in the collection of the Naturkundemuseum (Natural History Museum) in Lüneburg (pers. comm. R. Erbguth, 2013) and so their current whereabouts is unknown.

1910: Josef Pompeckj – Campanian of Haldem

The most complete cranial remains of a mosasaur found to date in Germany comprises a partial right maxilla with teeth and associated left postorbitofrontal and two pterygoid teeth (GZG.V.10024) found during a geological fieldtrip by the University of Göttingen in April 1908 and described by Josef Pompeckj in 1910. The original description by Pompeckj (Reference Pompeckj1910) also stated the presence of a cervical vertebra and rib fragments, although these elements are missing today.

Josef Felix Pompeckj (1867–1930; Fig. 6A) studied geology and palaeontology at the University of Königsberg (Kaliningrad) and subsequently held positions at various universities in Germany. His long and successful career included professorships at Hohenheim (from 1904), Göttingen (from 1907) and Tübingen (from 1913). Finally, in 1917, he was offered a position at the Friedrich-Wilhelms University (today Humboldt-University) in Berlin as professor of geology and palaeontology, and director of the associated Geologisch-Paläontologisches Museum (today the Museum für Naturkunde (Museum of Natural History)). In 1923 he became dean of his faculty and was elevated to rector of the university in 1925. He stayed at Berlin for the rest of his life (Hennig & Roethe, Reference Hennig and Roethe1930; Krüger, Reference Krüger2001).

The remains Pompeckj (Reference Pompeckj1910) described were found in Haldem (now a part of the community of Stemwede, North-Rhine Westphalia, northwestern Germany) in a yellowish sandy limestone of the uppermost Campanian Stemwede Formation (Fig. 6B). Pompeckj compared the maxillary fragment to various genera of mosasaurs and concluded that it showed closest similarities to Mosasaurus mosasauroides (originally Leiodon mosasauroides Gaudry, Reference Gaudry1892). This species, based on a skull fragment comprising the rostrad portions of the cranium and mandibles, from the Maastrichtian of the Basses-Pyrénées in southwestern France, is poorly known and may – based on the specialised, highly trenchant dental morphology – represent a distinct genus (Lingham-Soliar, Reference Lingham-Soliar and Sarjeant1993; LeBlanc et al., Reference LeBlanc, Caldwell and Bardet2012). Although sharing labiolingually compressed marginal teeth, this feature is much more pronounced in the French specimen, along with other differences (see Hornung & Reich, 2014). Lingham-Soliar (Reference Lingham-Soliar and Sarjeant1993) re-included L. mosasauroides in his concept of the genus Liodon (= Leiodon) and followed Pompeckj (Reference Pompeckj1910) in referring GZG.V.10024 tentatively to this species without further comments, a view that was repeated by Sachs (Reference Sachs2000).

A reassessment of the specimen showed that it is referable to the tylosaurine genus Hainosaurus Dollo, Reference Dollo1885 (for details see Hornung & Reich, Reference Hornung and Reich2014). Curiously, Pompeckj (1910, p. 125) compared the Haldem specimen also to this genus but dismissed a reference to it on the basis of differences in the tooth morphology. In fact, the dental morphologies are quite similar, however the teeth in Hainosaurus were described very inadequately until recently (Lindgren, Reference Lindgren2005).

In addition to the description of the Haldem specimen Pompeckj (Reference Pompeckj1910) also provided a summary of the contemporary knowledge on mosasaur morphology and habits. This is the most comprehensive work on their palaeobiology resulting from the discovery of a mosasaur in Germany until today. Aside from compiling the results from major works on mosasaurs, especially by Louis Dollo (1857–1931), Georg Baur (1859–1898), Edward Drinker Cope (1840–1897), John Campbell Merriam (1869–1945), Henry Fairfield Osborn (1857–1935), Samuel Wendell Williston (1852–1918), Dragutin Gorjanović-Kramberger (1856–1936) and Andreas Kornhuber (1824–1905), Pompeckj added his own ideas on mosasaurs, especially on the question of their palaeobiogeography and extinction. He paid special attention to locomotion, pointing out that the main locomotory organ was the tail, which mosasaurs might have used in meandering motions similar to newts. Furthermore, he concluded that the front limbs were used to steer and balance the position in the water, similar to bilge keels on ships. Other subjects included diving capacity, reproduction, feeding and relationships to aigialosaurs and extant lizards.

Most significantly, Pompeckj's essay on mosasaur palaeobiology is interwoven with a critical discussion of a then new phylogenetic theory, published by Gustav Steinmann two years earlier.

Johann Heinrich Conrad Gottfried Gustav Steinmann (1856–1929), born in Braunschweig (Brunswick), studied chemistry, mineralogy, geology and zoology at the universities of Braunschweig and Munich. He completed a doctoral thesis on fossil hydrozoans in 1877 and a habilitation on the regional geology of Bolivia in 1880. Following affiliations with the universities of Strasbourg and Jena, he was appointed professor in Freiburg im Breisgau in 1886. In 1906, Steinmann became head of the newly founded institute of geology and palaeontology at the University of Bonn, which he developed during the following years as an effective administrator (Wilckens, Reference Wilckens1930). Today, the institute bears his name and is still located in buildings that he commissioned.

He was an accomplished scientist, enormously productive and versatile in his fields. However, his ideas received a mixed reception. Although some parts of his work – especially in regional geology – are still considered groundbreaking, others have not found acceptance (Seibold & Seibold, Reference Seibold and Seibold2010) and may be considered eccentric.

In 1908 Steinmann published his book Die geologischen Grundlagen der Abstammungslehre (The Geological Foundations of the Theory of Descent), in which he proposed an unorthodox phylogenetic theory. Citing the alleged lack of species that are transitional in morphology between higher systematic categories, Steinmann denied the monophyletic origins and subsequent diversification of these groups. He regarded the higher categories (genera, families, etc.) as different ‘levels of organisation’ that were superimposed by changing environmental conditions to independently evolving, anagenetic successions of species (‘Abstammungslinien’ or ‘lines of descent’). Therefore he found characters defining and separating those higher categories not meaningful for the reconstruction of phylogeny but proposed to use features like external morphology or ornamentation for this purpose. He also considered extinction, as a natural phenomenon, extremely uncommon and an exception, suggesting that almost all fossil species are included as intermediate mutations somewhere in the chains of the lines of descent, leading to extant species.

As a consequence of those principles, he radically regrouped the organisms in a system he deemed to reflect serial and anagenetic phylogeny. This regrouping saw, for example, the ascidians (Tunicata) as a group of shell-less molluscs that had descended from rudistid bivalves (Steinmann, Reference Steinmann1908, p. 174ff.; in contrast Jaekel, Reference Jaekel1915, p. 67). This lineage was based on the superficial, entirely function-related, similarities between ascidians and rudists, and the desire to include the rudists in a persisting evolutionary lineage instead of being an extinct clade. However, he completely disregarded the numerous differences between those two groups that are not functional.

The same is true for the system he unfolded for the amniotes. He distinguished between the (extant), ‘primitive’ reptiles, in which he included the turtles, crocodilians, lizards and snakes, and the relatively advanced ‘metareptiles’. Within the reptiles, he saw an anagenetic continuity towards the turtles via rhynchosaurs and placodonts, while he assumed direct ancestry of the remainder within the non-amniote basal tetrapods (e.g. the genera Archegosaurus and Eryops for longirostrine and latirostrine crocodilians, respectively; Steinmann, Reference Steinmann1908, p. 214). The metareptiles were considered by him to represent the ancestors of birds and mammals. The distinction from the primitive reptiles was based on his – rather avant-garde – suggestion that the metareptiles, including dinosaurs, pterosaurs and various marine taxa, had elevated rates of metabolism and were potentially endothermic. With basal synapsids or therapsids not yet defined, he suggested that the metareptiles split into a dichotomy between the ancestors of birds (Avireptilia) and those of mammals (Mammoreptilia). Again he drew the line between the two entirely deliberately, for example he proposed the sauropod genus Diplodocus to have belonged to the Avireptilia, being a potential bird ancestor, while he referred the sauropod genera Cetiosaurus, ‘Camerosaurus’ (sic! = Camarasaurus), ‘Brontosaurus’ (= Apatosaurus) and ‘Morosaurus’ (= Camarasaurus) to the Mammoreptilia. He justified this by a ‘complete’ dentition in the latter, while Diplodocus had teeth only in the rostral part of the jaws (Steinmann, Reference Steinmann1908, p. 220).

Other ‘mammoreptiles’ included ceratopsians (which he renamed ‘Homoeopoda’), pterosaurs, ichthyosaurs, plesiosaurs and ‘thalattosaurs’. Theropods, ornithopods and stegosaurs were included in the Avireptilia (Steinmann, Reference Steinmann1908, p. 220f.).

Steinmann’s proposal – although claiming to solve inherent problems of the classical, monophyly-based theory – had a number of flaws. The most important of these were the opportunistic use or even total ignorance of the principle of homology and the employment of a highly random concept of homoplasy. The criteria to distinguish between phylogenetically relevant character transition and functionally induced convergence were entirely arbitrary and not justified.

With regard to mosasaurs, Steinmann hypothesised that they were an intermediate member in a phylogenetic lineage ranging from the Triassic ‘mammoreptilian’ thalattosaurs (which he expanded to include mosasaurs) to extant baleen whales (Mysticeti) based on a rough comparison of cranial features such as a rounded occiput, oblique nasal ducts, a flexible mandibular symphysis and similar morphology of the quadrate in ‘thalattosaurs’ and the bulla tympanica in whales. He also cited reduced metapodials, weak hyperphalangy and absence of polyphalangy in the forelimb as shared characteristics. He brought forward similar arguments to link plesiosaurs phylogenetically with toothed whales (Odontoceti), and ichthyosaurs with dolphins (Delphinoidea).

Pompeckj (1910, p. 132ff.) rejected a phylogenetic linkage of mosasaurs either to the Triassic Thalattosauria or to cetaceans. He pointed out that the alleged ’synapomorphies‘ in the cranial morphology between these clades are also present in other mammal groups or were wrongly identified. With regard to the vertebral series and forelimbs, he argued that those of mosasaurs show major differences to those of whales, which cannot be explained by environmental changes, as the locomotory requirements of mosasaurs and whales were essentially the same. As the most important argument he cited the differences in the proportions of the forelimbs, with whales having a proportionally much more elongate zeugopodium, which would have required an inexplicable reversal from the short zeugopodium in mosasaurs. He stated that it is more parsimonious to deduce forelimb morphology in whales from terrestrial mammals than from marine reptiles.

Pompeckj (Reference Pompeckj1910) also delved into possible reasons for mosasaur extinction. Listing the known temporal and spatial relationships of mosasaur occurrences known at this time, he considered a shift of mosasaur localities through time and therefore a ‘wandering’ of the presence of mosasaurs across the globe (a view which cannot be upheld by present-day data). He proposed that their occurrence was bound to shallow, coastal regions (which is probable, although there may be a certain preservational bias for pelagic deposits). After considering potential but hypothetical environmental changes (especially to fluvial environments, which he had proposed as spawning grounds), increased predatory pressure by actinopterygians to juvenile mosasaurs, feeding competition by sharks or ‘disadvantageous’ gigantism, he considered these possibilities as conjectural or insufficient. In conclusion he saw the most probable reason for the extinction in an ‘over-specialisation’, hypothesising a ‘depletion’ of a somehow predetermined reservoir of the Umprägungsfähigkeit (ability to transform) of species. He envisaged a natural ‘expiry’ of taxa rather than their ‘annihilation’ (Pompeckj, Reference Pompeckj1910, p. 140).

The specimen from Haldem was incorporated in the Göttingen collections, where Pompeckj was professor of geology and palaeontology at the time of the discovery. A few decades later, his successor Othenio Abel (1875–1946) undertook a major effort to renew an inclusive view of the fossil biosphere, coining (together with Louis Dollo) the concept of palaeobiology. In his function as the head of the palaeontological department in Göttingen, he also fostered the popularisation of these concepts by designing an exhibit on palaeobiology and he commissioned the Austrian painter, sculptor and palaeoartist Franz Roubal (1889–1969) to create a series of large formatted paintings and sculptures of extinct animals (Reich & Reitner, Reference Reich, Reitner, Reitner, Reich and Schmidt2004). One of these was a reconstruction of a mosasaur hunting on sharks, created in 1937 (Fig. 6C) and published by Abel (Reference Abel and Berger1939). Today the specimen is on display at the Geoscience Museum at Göttingen (Reich et al., Reference Reich, Reitner, Roden and Stegemann2013), next to the framed oil painting by Roubal.

1915: Karl Gripp – Coniacian to Campanian of Lägerdorf

In 1915 Karl Christian Johannes Gripp (1891–1985) published a note on a series of mosasaur vertebrae found in Lägerdorf, Holstein. Gripp studied geology at Göttingen, Kiel and Grenoble. From 1927 to 1934 he was professor of geology at the University of Hamburg. From 1940 to 1958 Gripp was affiliated with the University of Kiel, where he eventually became director of the Geological Institute. Gripp's research focused mainly on Quaternary geology, but he also published several books on the regional geology of northern Germany (e.g. Gripp, Reference Gripp1933, Reference Gripp1964). Furthermore, he had a lifelong interest in Arctic geology and participated in expeditions to Svalbard and Greenland (von der Brelie, 1985; Prange, Reference Prange1991). In 1927 Gripp was a member of an expedition to Svalbard, which discovered parts of an enigmatic Lower Triassic ichthyosaur that Wiman (Reference Wiman1928) named Grippia longirostris in honour of Karl Gripp. Gripp (Reference Gripp1915) mentioned a series of 19 procoelous, laterally compressed caudal vertebrae. He did not present a formal description nor an illustration, but noted a similarity to the caudal vertebrae of Mosasaurus. The specimen was donated to the Museum of Mineralogy and Geology at Hamburg, but is not present in the collection of the Institute of Geology and Palaeontology in Hamburg (S. Sachs, pers. obs., 2012). Thus, these vertebrae were probably destroyed in 1943, as were other specimens housed in the geological institute in Hamburg (see also Hillmer, Reference Hillmer2006, p. 3). The exact age of the vertebrae cannot be provided because the strata exposed at Lägerdorf range from the Middle Coniacian to the Upper Campanian (Schulz et al., 1984) and Gripp (Reference Gripp1915) did not provide stratigraphic information.