recursal/Fanatic-Fandom huggingface dataset:
1841 Vertebrate Paleontology Reference List

**1831 1832 1833 1834 1835 1836 1837 1838 1839 1840 1842 1843 1844 1845 1846 1847 1848 1849 1850 1851**

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**1. **Agassiz, Louis** (1841) - [Note on fossil jaw, on which is based the genus Phocodon, type P. scillae Ag.].
*Valentin's Repertorium f. Anat. Physiol.*, VI, p. 236.**

**2. **Agassiz, Louis** (1841) - On the fossil fishes found by Mr. Gardner in the Province of Ceará, in the North of Brazil.
*The Edinburgh New Philosophical Journal*, 30:82-84.**

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**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-24 **Last updated:** 2018-08-03
1573 Vertebrate Paleontology Reference List

**1563 1564 1565 1566 1567 1568 1569 1570 1571 1572 1574 1575 1576 1577 1578 1579 1580 1581 1582 1583**

* B-1

**1. Bacci, Anddrea (1573) - *L'Aiicorno*.
 - Florence, vi + 80 pp.
 - Venice, 1566
 - Rome, 1587
 - Stuttgart, 1598.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-28 **Last updated:** 2018-06-03
1557 Vertebrate Paleontology Reference List

**1547 1548 1549 1550 1551 1552 1553 1554 1555 1556 1558 1559 1560 1561 1562 1563 1563 1564 1566 1567**

* C-1

**1. Cardanus, Hieronymus (1557) - *De rerum varietate libri XVII*.
Fol., Basel. xi + 707 pp. + index.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-04-18 **Last updated:** 2018-06-03
1903 Vertebrate Paleontology Reference List

**1893 1894 1895 1896 1897 1898 1899 1900 1901 1902 1904 1905 1906 1907 1908 1909 1910 1911 1912 1913**

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* A-10
* B-0
* C-0
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* L-0

**1. **Abel, Othenio** (1903) - Die fossilen Sirenen des Wiener Beckens.
*Verh. Geol. Reichsanst. Wien*, 1903: 72**

**2. **Abel, Othenio** (1903) - Exkursion nach Heiligenstadt, Nussdorf und auf den Kahlenberg.
*Internat. geol. Congr., Vienna. Führer für die geologischen Exkursionen in Oesterreich*. IX 8 pp.**

**3. **Abel, Othenio** (1903) - Zwei neue Menschenaffen aus den Leithakalkbildungen des Wiener Beckens.
*Centralbl. Min. Geol. Pal.*, 1903 176-182.**

**4. Adams, Lionel E. (1903) - A contribution to our knowledge of the mole (Talpa europoea).
*Mem. Manchester Soc.*, XLVII 1-39, 28 text-figs.**

**5. Adloff, Paulf (1903) - Zur Frage nach der Entstehung der heutigen Säugethierzahnformen.
*Zeitschr. Morphol. Anthrop.*, V 357-382, pl. x, 5 text-figs.**

**6. Adloff, Paul (1903) - *Kiefer und Zähne in ihrer Bedeutung für die Anthropologie*.
Wiener zahnärztliche Monatsschrift.  Vienna V 383-394.**

**7. Albrecht, O. (1903) - *Zur ältesten Geschichte des Hundes*.
Diss., Munich. 63 pp.**

**8. Allen, J.A. (1903) - Report on the mammals collected in northeastern Siberia by the Jesup North Pacific expedition, with itin erary and field notes, by N. G. Buxton.
*Bull. Amer. Mus. Nat. Hist.*, XIX 101-184.**

**9. Allis, Edward Phelps (1903) - On certain features of the lateral canals and cranial bones of Polyodon folium.
*Zool. Jahrb., Anat.*, XVII 659-678, pl. xxviii, 2 text-figs.**

**10. Allis, Edward Phelps (1903) - The skull and the cranial and first spinal muscles and nerves in Scomber scomber.
*Jour. Morphol.*, XVIII 45-308, pls. iii-xii.**

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**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-24 **Last updated:** 2018-08-07
1546 Vertebrate Paleontology Reference List

**1536 1537 1538 1539 1540 1541 1542 1543 1544 1545 1547 1548 1549 1550 1551 1552 1553 1554 1555 1556**

* L-1

**1. Lazius, Wolfgang (1546) - *Rerum Viennensium comentarii in quatuor libris distincti*.
Fol., Basel. 10 + 159 + 17 pp.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-04-10 **Last updated:** 2018-06-18
A New Parareptile (Parareptilia, Lanthanosuchoidea) from the Early Permian of Oklahoma

**1** **2** ****3**** **4** **5** **6** **7** **8** **9** **10** **11** **12** **13** **14** **15** **16** **17** **18** **19** **20** **21** **22** **23**

* Description
* Abstract
* Described species ( )
* References (49)

**An exquisitely preserved skull of *Feeserpeton oklahomensis*, gen. et sp. nov., collected from the Lower Permian fissure-fill deposits near Richards Spur, Oklahoma, is the newest parareptile from the locality. The specimen comprises an almost complete skull, lacking most of the premaxillae, parts of the jugals, and parts of the braincase. The maxillae and dentaries possess caniniform regions, including large caniniform teeth that are at least twice as large as any other tooth in the jaws. A phylogenetic analysis of Parareptilia that includes the new taxon indicates that the Early Permian F. oklahomensis is a member of the poorly known Lanthanosuchoidea, positioning it as the sister taxon of a clade consisting of *Acleistorhinus pteroticus* and *Lanthanosuchus watsoni*. This new taxon adds significantly to our limited knowledge of the early stages of parareptile evolution, as well as the large terrestrial tetrapod diversity found at Richards Spur.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-03-08 **Last updated:** 2021-12-28
1556 Vertebrate Paleontology Reference List

**1546 1547 1548 1549 1550 1551 1552 1553 1554 1555 1557 1558 1559 1560 1561 1562 1563 1563 1564 1566**

* A-2

**1. Aldrovandi, Ulysse (1556) - *Delle statue antiche che per tutta Roma...si veggono*.
In: Mauro, Lucio, l'Le antichita della citta di Roma." Venice (1556).**

**2. Augustinus, Aurelius (1556) - *Quintus tomus operum divi Aurelii Augustini hipponensis episcopi, continens de clvitate dei libros XXII. ad priscae venerandaeque vetustatis exemplaria denuo collatos, eruditissimisque insuper commentariis per undequaque doctis. virum Joan. Lodovicum vivem illustratos et recognitos*.
Fol., Basel, 878 pp.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-04-18 **Last updated:** 2018-06-03
Devonian filter-feeding sharks

**1** **2** **3** **4** ****5**** **6** **7** **8** **9** **10** **11** **12** **13** **14** **15** **16** **17** **18** **19** **20** **21**

* Description
* abstract
* Described species ( )
* New species ( )
* References (13)

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-07-09 **Last updated:** 2018-07-10
1509 Vertebrate Paleontology Reference List

**1546 1547 1548 1549 1550 1551 1552 1553 1554 1555 1556 1557 1558 1559 1560 1561 1562 1563 1564 1565**

* F-1

**1. Fregoso, Battista (1509) - *De dictis factisque memorabilibus collectanea*.
Fol., Milan.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-04-10 **Last updated:** 2018-06-18
Вагон для Арни

**Вагон для Арни** — первая половина двадцатого эпизода второго сезона.

## Сюжет

Бадди и Тайни с матерью едут на Поезде Динозавров к Аргентинозаврам. Тайни и Бадди при этом поясняет Кондуктору, что самого большого решили оставить напоследок. Кондуктор подтверждает, что Аргентинозавры самые большие динозавры, и также говорит, что когда Арни вырастет, то он будет размером более двух пассажирских вагонов. Бадди и Тайни решили помолчать перед Арни насчет слов о поезде, так как ему будет очень грустно.

Прибыв на станцию «Пастбища Аргентинозавров», там Бадди и Тайни приветствует Арни. Потом Бадди и Тайни с матерью встретили отца Арни, и он говорит им, что их не беспокоят хищники, так они очень большие. Потом Дасплетозавр приготовился нападать на Мистера Аргентинозавра, но из-за большого размера, он отказался от этих действий.

Бадди и Тайни стали проводить время с Арни, играя с ним в прятки. Потом они отправились на станцию, где наблюдали за прибытием поезда. Бадди и Тайни с матерью стали отправляться домой на поезде, во время пути Бадди и Тайни загрустили из-за того, что Арни не может прокатиться на поезде.

Прибыв на станцию «Город Троодонов», Бадди и Тайни стали рассматривать депо, где находятся различные вагоны, там Тайни пришло в голову идея, создать специальный вагон для больших зауроподов.

Вскоре на станцию «Пастбища Аргентинозавров» прибывает поезд с новым специальным вагоном для Зауроподов, куда на нём садится Арни и с ними отправляются в путешествие на поезде, а Бадди и Тайни напевают песню «Огромный динозавр».
1843 Vertebrate Paleontology Reference List

**1833 1834 1835 1836 1837 1838 1839 1840 1841 1842 1844 1845 1846 1847 1848 1849 1850 1851 1852 1853**

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* B-0
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* J-0
* K-0
* L-0

**1. **Agassiz, Louis** (1843) - Report on the fossil fishes of the Devonian system or Old Red sandstone.
*Report Brit. Assoc. Adv. Sci.*, 12th meeting, Manchester, 1842, pp. 80-88.**

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**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-24 **Last updated:** 2018-08-03
1993 Vertebrate Paleontology Reference List

**1983 1984 1985 1986 1987 1988 1989 1990 1991 1992 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003**

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**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-06-30 **Last updated:** 2018-06-30
1799 Vertebrate Paleontology Reference List

**1789 1790 1791 1792 1793 1794 1795 1796 1797 1798 1800 1801 1802 1803 1804 1805 1806 1807 1808 1809**

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* C-4
* F-1
* G-1
* J-1

**1. Anonymous (1799) - Dodo.
*Naturalists' pocket magazine; or, Compleat cabinet of the curiosities and beauties of nature*.
 London I (9) 1-4, pl.**

**1. Blumenbach, Johann Friedrich (1799) - *Handbuch der Naturgeschichte*.
6th ed., Göttingen. xvi + 708 pp., 2 pls.**

**1. Camper, Adrian Gilles (1799) - Over den oorsprong der uitgedolven beenderen van den St. Pietersberg, b Maestricht.
*Natuurk. Verh. Holland. Maatsch. Wet.*, I 169-198, 2 pls.**

**2. Cuvier, Georges (1799) - Extrait d'un mémoire sur les ossemens fossiles de quadrupèdes.
*Bull. Soc. philom. Paris*, I 2 137-139.**

**3. Cuvier, Georges (1799) - Mémoir sur les espèces d'éléphans vivants et fossiles.
 *- Mém. de l'Institut Nat. Sci. et Arts*, ii pp. 1-22, pls. ii-vi.
 *- Mém. Acad. Sci. Paris*, II 1-22, pls. II-VI.**

**4. Cuvier, Georges (1799) - Sur les ossements qui se trouvent dans le gypse de Montmartre.
*Bull. Soc. philom. Paris*, I 2 154-155.**

**1. Faujas de Saint-Fond, Barthélemy (1799) - *Histoire naturelle de la montagne de Saint-Pierre de Maestricht*.
 4, Paris. 263 pp., 54 pls.**

**1. G. A. (1799) - Fish teeth found between Newmarket and Bury.
*Gentleman's Mag.*, LXIX 12-13.**

**1. Jefferson, Thomas (1799) - A memoir on the discovery of certain bones of a quadruped of the clawed kind in the western parts of Virginia.
*Trans. Amer. Philos. Society*, iv pp. 246-260.**

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* S-1
* T-1
* V-1
* W-1

**1. Rosenmüller, J.C. & Tilesius, A. von (1799) - *Beschreibung merckwürdiger Höhlen*.
Leipzig. xvi + 294 pp., 10 pls.**

**2. Roume (1799) - Squelette fossile trouvé sur les bords de la Plata.
*Bull. Soc. philom. Paris*, I (2) 96-97.**

**1. Saint Fond, F. (1799) - *Head of the Crocodile* p. 59-67
Historie Naturelle de la Montage de Saint-Pierre de Maestricht.**

**1. Turner, George (1799) - Memoir on the extraneous fossils denominated mammoth bones; principally designed to show that they are the remains of more than one species of nondescript animal.
*Trans. Amer. philos. Soc.*, IV 510-518.**

**1. Vauquelin (1799) - Analyse der fossilen Knochen von Montmartre.
*Allgemeines Journal der Chemie.*, Berlin III 264.**

**1. Wistar, Caspar (1799) - A description of the bones deposited by the president in the museum of the society, and represented in the annexed plates.
*Trans. Amer. Philos. Soc.*, iv pp. 526-531, with 2 pls.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-04-19 **Last updated:** 2018-08-03
A new Basal Porpoise, Pterophocaena nishinoi (Cetacea, Odontoceti, Delphinoidea), from the Upper Miocene of Japan and its Phylogenetic Relationships

**1** **2** **3** **4** **5** **6** **7** **8** **9** **10** **11** **12** **13** **14** ****15**** **16** **17** **18** **19** **20** **21** **22** **23**

* Description
* Abstract
* Described species( )
* References (74)

***Pterophocaena nishinoi*, gen. et sp. nov. (Phocoenidae), from the upper Miocene Wakkanai Formation (9.2–9.3 Ma) in Hokkaido, northern Japan, is described. This is the oldest fossil phocoenid in the western North Pacific, thus extending the fossil record of Phocoenidae an additional approximately 4 million years in the region compared with the previous record. The holotype, composed of a partial skull, with right periotic and tympanic bulla and a postcranial skeleton, has the following apomorphic characters: absence of the premaxillary eminence; posterior half of the hamular process of the pterygoids not separated by palatines; prominent dorsolaterally projecting premaxilla in the facial area; supraorbital process of the maxilla steeply sloping ventrolaterally; posteriorly protruding temporal crest; anteroventrally narrowed and inverted teardrop-shaped temporal fossa; and several short ridges on the tympanosquamosal recess of the squamosal. A comprehensive cladistic analysis (66 ingroup taxa and 278 morphological characters) indicates that *Pterophocaena* is the most basal phocoenid yet discovered, and that Phocoenidae and Delphinidae are closely related. The discovery of *Pterophocaena* leads to a review of previous hypotheses for the origin of Phocoenidae, and indicates that phocoenids had already diversified in the Pacific Ocean by late Miocene.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2017-04-09 **Last updated:** 2021-12-28
A New Osteostracan Fauna from the Devonian of the Welsh Borderlands and Observations on the Taxonomy and Growth of Osteostraci

**1** ****2**** **3** **4** **5** **6** **7** **8** **9** **10** **11** **12** **13** **14** **15** **16** **17** **18** **19** **20** **21** **22** **23**

* Description
* Abstract
* Described species ( )
* References (55)

**The Osteostraci are a morphologically diverse group of jawless fishes considered as sister taxon to jawed vertebrates. Fossil Osteostraci therefore have wide-reaching ramifications for our understanding of the origin and evolution of gnathostomes. Their utility in this context is currently impeded by rudimentary taxonomy of faunas from the United Kingdom. Principal among these is a well-preserved, previously undescribed fauna from the Early Devonian (Lochkovian) of Wayne Herbert Quarry, Herefordshire. Here we provide a description of new osteostracan material from this fauna. Anatomical observations of the character-rich, taxonomically informative headshield, combined with quantitative measurements, have permitted identification of 15 variable characters. From these, seven discrete morphogroups are recognized and used to establish the taxonomy of the material. This includes two new species of Zenaspididae (*Zenaspis waynensis* and *Diademaspis janvieri*), two new species of Cornuata incertae sedis (*Janaspis newtonensis* and *J. punctata*), two indeterminate species, and Pattenaspis whitei, which is redescribed on the basis of new material. Our analyses indicate that cornuate osteostracan species are likely over-split due to erection of new taxa based on poorly preserved type specimens, inadequate consideration of taphonomic character loss, and over-reliance on continuous rather than discrete characters. Furthermore, patterns of dermoskeleton ornamentation and tessellation of Diademaspis janvieri and Cornuata, gen. indet., sp. B are used to infer mechanisms of dermoskeletal growth. These new data allow incorporation of this fauna into scenarios of osteostracan evolution, considerations of gnathostome origin, and studies of global Lochkovian diversity.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-03-08 **Last updated:** 2021-12-29
1550 Vertebrate Paleontology Reference List

**1540 1541 1542 1543 1544 1545 1546 1547 1548 1549 1551 1552 1553 1554 1555 1556 1557 1558 1559 1560**

* M-1

**1.Münster, Sebastian (1550) - *Cosmographiae universalis*. Lib. VI. Fol.,
Basel. 1162 pp., illus.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-04-18 **Last updated:** 2018-06-18
A new species of the surgeon fish genus Tauichthys from the Eocene of Monte Bolca, Italy (Perciformes, Acanthuridae)

* Description
* Abstract
* Described species ( )
* New species (1)
* References ( )

***Tauichthys aspesae* differs from the previously described species, *T. padremenini*, by having the derived condition of the edges of the teeth highly lobate, rather than smooth as in *T. padremenini*, and in the number of soft rays in the dorsal and anal fins. The single known specimens of both species ofTauichthys have acronurus pre-settlement stage features: vertically elongate scales, black peritoneum, serrations on the second dorsal- and anal-fin spines, and, in the case ofT. aspesae, on some of the head bones**.

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-13 **Last updated:** 2018-05-13
1801 Vertebrate Paleontology Reference List

**1791 1792 1793 1794 1795 1796 1797 1798 1799 1800 1802 1803 1804 1805 1806 1807 1808 1809 1810 1811**

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* A-2
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* C-3
* D-1
* E-0
* F-1
* G-1
* H-1
* I-0
* J-0
* K-1
* L-0

**1. Anonymous (1801) - Ueber die aus der Erde gegrabenen Säugthiere.  Dabei ein Auszug der Ankündigung eines Werkes des Professors Cuvier.
*Neue berlinische Monatsschrif*, VI 3-23.**

**2. Azara, F. de (1801) - *Essais sur l’Histoire Naturelle des Quadrupèdes de la Province du Paraguay*.
Vol. 2. C. Pougens, Paris. 499 pps.**

**1. Bloch, M.E. & Schneider, J.G. (1801) - *Systema Ichthyologiae iconibus cx illustratum. Post obitum auctoris opus inchoatum absolvit, correxit, interpolavit. Sumtibus Auctoris Impressum et Bibliopolio Sanderiano Commissum*.
Berlin, i-lx + 584 pp., 110 pls.**

**1. Cuvier, Georges (1801) - Extrait d'un mémoire sur les dents des poissons.
*Bull. Soc. Philom.*, Paris III 25-26.**

**2. Cuvier, Georges (1801) - Extrait d'un ouvrage sur les espèces de quadrupèdes dont on a trouvé les ossemens dans l'intérieur de la terre.
*Jour. Phys. Chim. Hist. nat. Arts*, LII 253-267.**

**3. Cuvier, Georges (1801) - Nouvelles découvertes d'os fossiles.
*Bull. Soc. philom.*, Paris. III 17.**

**1. Delamétherie, Jean-Cla (1801) - Sur la tête fossile d'un grand animal, trouvée dans des gypses, auprès de Méaux.
*Jour. Phys. Chim. Hist. nat. Arts*, LIII 403-404.**

**1.**

**1. Fortis, Giovanni Battista Al (1801) - Lettre à J.-C. Dela therie (on ornitholiths and other fossils).
*Jour. Phys. Chim. Hist. nat. Arts*, LII 320-322.**

**1. Graham, James C. (1801) - Further account of fossil bones in Orange and Ulster Counties (N. Y.).
*Med. Reposit. N. Y.*, IV 213-214.**

**1. Häfeli (1801) - Nachricht von einigen fossilen Ueberresten eines Rhinoceros, und einer Missgeburt von einem Karpfen.
*Mag. neuest. Zustand Naturk.*, III 512-516.**

**1.**

**1.**

**1. Köcher (1801) - Die Höhle bei Glücksbrunn.
*Mag. ges. Mineral.*, I 428-440, pl.**

**1.**

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**1. Miller, Sylvanus (1801) - Account of large bones dug up in Orange County (State of New York).
*Med. Reposit. N. Y.*, IV 211-213.**

**1.**

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**1. Roxburgh (1801) - An Account of a new Species of Delphinus, an Inhabitant of the Ganges.
*Asiat. Res. Trans. Soc.*, 1801; 7(4):170-174.**

**1.**

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**1.**

**1. von Hoff, Karl Ernst Adolf (1801) - Ueber die Arten der Säugetiere, von welchen man Knochen im Innern der Erde findet.  Eine Aufforderung des Br. Geo. Cuvier an die Gelehrten und Freunde der Wissenschaften.
*Mag. ges. Min*, I 449-469.**

**2. von Hoff, Karl Ernst Adolf (1801) - Ueber die Ornitholithen.
*Mag. ges. Mineral.*, I 283-302, pl.**

**1. Warner, Richard (1801) - The history of Bath.
4, Bath. 402 + 123 pp.**

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**Created :** 2018-04-07 **Last updated:** 2018-06-03
1992 Vertebrate Paleontology Reference List

**1982 1934 1984 1985 1986 1987 1988 1989 1990 1991 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002**

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**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-06-30 **Last updated:** 2018-08-03
1905 : Le terrain nummulitique du Bassin de l'Adour

**1** **2** **3** **4** **5** **6** **7** **8** **9** **10** **11** **12** **13** **14** **15** **16** **17** **18** **19** **20** **21** **22** **23** **24** **25** **26** **27** **28** **29** **30** **31** **32** **33** **34** **35** **36** **37** **38** **39** **40** **41** **42** **43** **44** **45** **46** **47** **48** **49** **50** **51** **52** **53** **54** **55** **56** **57** **58** **59** **60** **61** **62** **63** **64** **65** **66** **67** **68** **69** **70** **71** **72** **73** **74** **75** **76** **77** **78** **79** **80** **81** **82** **83** **84** **85** **86** **87** **88** **89** **90** **91** **92** **93** **94** **95** **96** **97** **98** **99** **100** **101** **102** **103** **104** **105** **106** **107** **108** **109** **110** **111** **112** **113** **114** **115**
Evolutionary divergence in the feeding mechanism of fishes

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* Description
* abstract
* Described species ( )
* New species ( )
* References (34)

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-07-08 **Last updated:** 2018-07-12
Sea-surface dynamics and palaeoenvironmental changes in the North Atlantic Ocean (IODP Site U1313) during Marine Isotope Stage 19 inferred from coccolithophore assemblages.

**1** **2** **3** **4** **5** **6** **7** ****8**** **9** **10** **11**
* Description
* Abstract

**The end of the glacial MIS 20 is marked by the arrival of cold waters, deriving from ice melting at higher latitudes, as recorded by Coccolithus pelagicus pelagicus. The MIS 19c is characterised by an extension of warmer North Atlantic Transitional Waters (NATW) reflecting the intensification of subtropical gyre influence on Site U1313, identified by an increase in warm species Umbilicosphaera sibogae. The influence on the site of cooler NATW is inferred from higher percentages of Gephyrocapsa margereli, which starts increasing from ~ 779 ka. Finally, the transition from MIS 19a to MIS 18 is characterised by a southward shift of the palaeoceanographic system due to a southward extension of the subpolar front, as indicated by an increase of cold subspecies *C. pelagicus pelagicus*.**
**The evolution of the palaeoproductivity proxy records (number of coccoliths/g of sediment and Nannofossil Accumulation Rate — NAR) and the abundances of small *Gephyrocapsa*, *G. margereli*, *U. sibogae* and *C. pelagicus pelagicus* show that fluctuations in sea-surface productivity and alternations between cooling and warming phases occurred on the precessional timescale.**
**Spectral analyses of U. sibogae, number of coccoliths/g of sediment and NAR indicate a significant concentration of variance close to half precession (~ 10 kyr); this reflects a nonlinear response of the mid-latitude North Atlantic surface ocean to low-latitude insolation forcing.**
**Furthermore, millennial to multi-centennial instability in sea-surface dynamics is highlighted by spectral and wavelet analyses of *U. sibogae*, *G. margereli* and *C. pelagicus pelagicus* percentages, number of coccoliths/g of sediment and NAR, which reveal the occurrence of rapid events, related to stadial and interstadial-type conditions.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-03-26 **Last updated:** 2021-12-31
1853 Vertebrate Paleontology Reference List

**1843 1844 1845 1846 1847 1848 1849 1850 1851 **1853** 1854 1855 1856 1857 1858 1859 1860 1861 1862 1863**

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**1. **Agassiz, Louis** (1853) - Notice of Joseph Leidy's "Memoir of the extinct species of American ox".
*Amer. Jour. Sci.*, (2), xvi, p. 281**

**2. American Journal of Science (1853) - Notice of the "Mastodon giganteus" of Dr. J. C. Warren.
*Amer. Jour. Sci.*, XV, pp. 367-373**

**3. American Journal of Science (1853) - Fossil elephant.
*Amer. Jour. Sci.*, (2), XV, p. 146**

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**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-20 **Last updated:** 2018-08-03
1559 Vertebrate Paleontology Reference List

**1549 1550 1551 1552 1553 1554 1555 1556 1557 1558 1560 1561 1562 1563 1563 1564 1566 1567 1568 1569**

* M-1

**1. Matthioli, Petrus Andreas (1559) - *Commentarii secundo aucti, in libros sex Pedacci Dioscoridis Anazarbei de medica materia*.
Fol., Venice. 98 + 776 pp. 1st ed., 1554.**

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**Created :** 2018-04-18 **Last updated:** 2018-06-03
Additions to the elasmobranch fauna from the upper Cretaceous of New Jersey (middle Maastrichtian, Navesink Formation)

* Description
* Abstract
* Described species (3)
* New species (1)
* References (42)

**Three additional taxa are also described : Heterodontus creamridgensis, Squalicorax sp. and Pseudocorax affinis which is noted for the first time in North America.**
**The whole elasmobranch fauna of the Early Maastrichtian localities of New Jersey is reevaluated and several generic assignments are changed in comparison to the list previously published in 1975 (Cappetta & Case).**

 **2** | ***Pseudocorax aff. affinis* MÜNSTER in AGASSIZ, 1843** | 9-10
 **3** | ***Squalicorax* sp.** | 10

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**Created :** 2016-03-17 **Last updated:** 2021-12-31
New data on chondrichthyan microremains from the Givetian of the Renanué section in the Aragonian Pyrenees (Spain)

**1** **2** **3** **4** **5** **6** ****7**** **8** **9** **10** **11** **12** **13** **14** **15** **16** **17** **18** **19** **20** **21**

* Description
* abstract
* Described species ( )
* New species ( )
* References (21)

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-07-10 **Last updated:** 2018-07-11
New gadiform otoliths from the Tertiary of the North Sea Basin and a revision of some fossil and recent species

* Description
* Abstract
* Described species (22)
* New species (10)
* References (43)

**Three new genera are established: *Protocolliolus, Neocolliolus and Palaeoraniceps*. Type material of some fossil otoliths of Gadidae described by Koken (1884, 1891) has been studied; as a result some systematic errors are corrected.**
**The existence of two recent species of coal-fishes (*Pollachius virens* (L.) and *Pollachius carbonarius* (L.)) is ascertained by study of their otoliths.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-03 **Last updated:** 2022-01-02
Fish otoliths from the pre-evaporitic (Early Messinian) sediments of northern Italy: their stratigraphic and palaeobiogeographic significance

* Description
* Abstract
* Described species (53)
* New Species (3)
* References (60)

**These results are in good agreement with the evolutionary trends documented for the Oligocene and Miocene teleost fauna, specifically an increase in percentage of genera inhabiting the modern Mediterranean, a very high percentage of Atlantic and Indo-Pacific genera, and a slight fall of the importance of present-day Indo-Pacific genera from the Rupelian up to the Late Miocene. Analysing the composition of the Early Messinian fauna at the level of nominal species indicates that about 53% of the species represented in the assemblages are still living in the Recent Mediterranean, and that a significant number of these were already present in the Tortonian. It is interesting that these species are mainly neritic. This seems to confirm that the close affinity of the fossil assemblage with the present-day Mediterranean neritic fauna, which was already recorded at the genus level for the Rupelian fauna, persists during the Neogene and continues until the Pleistocene.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-03-16 **Last updated:** 2020-01-21
Dermal denticle patterning in the Cretaceous hybodont shark Tribodus limae (Euselachii, Hybodontiformes), and its implications for the evolution of patterning in the chondrichthyan dermal skeleton

****1**** **2** **3** **4** **5** **6** **7** **8** **9** **10** **11** **12** **13** **14** **15** **16** **17** **18** **19** **20** **21** **22** **23**

* Description
* Abstract
* Described species ( )
* New species ( )
* References (72)

**As in modern elasmobranchs (sharks and rays), the shagreen of the hybodontiform shark *Tribodus limae* (Santana Formation, Aptian-Albian, Lower Cretaceous, northeastern Brazil) consists of non-growing (monodontode) dermal denticles that were shed, replaced, and supplemented by new ones during life. In modern elasmobranchs, these denticles are usually represented by a single size class (considered here to be the default arrangement), although larger denticles are sometimes present locally (e.g., thorn rows on the head and trunk in batomorphs). In Tribodus, however, the shagreen consists of two distinct morphological denticle types and size classes (two-size), both widely distributed over the body and fins, with smaller denticles overlying the bases of larger thorns as well as occupying areas between them. Using two conceptually distinct variants of a two-layer reaction-diffusion (R-D) simulation that is consistent with morphogen exchange across the basal lamina between the epidermal and dermal layers, we recovered two-size spatial arrangements similar to the Tribodus shagreen. Our results suggest that denticle patterning in the dermal skeleton of sharks can be replicated using R-D models with kinetics similar to those previously applied to a known mechanism of feather bud patterning in birds and to skin pigmentation patterning in modern teleost fishes. Reaction-diffusion simulations operationalize Reif's ‘odontode regulation theory,’ and so have an important conceptual place in the history of research on the dermal skeleton. Such a modeling framework may enable conceptual links to be drawn among seemingly disparate denticle arrays in Paleozoic and recent chondrichthyans, thereby guiding future work on the molecular and histological underpinnings of dermal skeleton development and evolution.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-04-26 **Last updated:** 2018-06-10
Selaciens nouveaux de l'Albien superieur de Wissant (Pas-de-Calais).

* Description
* Abstract
* New species ( )
* Described species ( )
* References ( )

**Screening in the Albian of Wissant area has allowed to collect an interesting selachian fauna including some new elements: *Orectoloboides* nov. gen., *Scyliorhinus destombesi* nov. sp. and *Protosqualus sigei* nov. gen., nov. sp.. The relationships of these forms are discussed.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-03-27 **Last updated:** 2018-06-10
Fish otoliths from the lower Tertiary of Ellesmere Island

* Description
* Abstract
* Described species (3)
* New species (2)
* References (25)

**Fish otoliths of five species are present in lower Tertiary (Paleocene to Lower Eocene) rocks at Strathcona Fiord, Ellesmere Island. Two species are new, one is conspecific with a species known from the Lower Eocene of southern England, and two remain in open nomenclature. Paleobiogeographic and other implications of the fauna are that first, there is no resemblance to central European faunas; second, there is a resemblance to northern European faunas from Great Britain and the Soviet Union, pointing to cooler climatic conditions; and third, composition of the fauna suggests the prevalence of deeper shelf conditions.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2017-11-22 **Last updated:** 2018-05-31
Sur la faune ichthyologique d’un falun dans l’Argile des Flandres près de Courtrai (Belgique)

* Description
* Résumé
* Described species (0)
* New species (0)
* References (32)

**Les Téléostéens se sont révélés comme des fossiles d'une grande valeur stratigraphique, et la coupure faunique avec la formation de Landen, aussi bien que celle avec la formation de den Hoorn (sables d'Aalter et d'Oedelem) est très nette. En plus, on remarque que les Téléostéens de l'argile des Flandres ont des affinités assez importantes avec ceux du London Clay**.

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-07-23 **Last updated:** 2018-07-27
Fisch-Otolithen aus der Typuslokalitat der Obermiozanen Sylt-Stufe (Morsum-Kliff, Insel Sylt, Nordwestdeutschland)

* Description
* Abstract
* Described species (33)
* New species (15)
* References (55)

**None was previously known from this locality.Descriptions of 14 new species from Sylt: Congridarura acutirostris, Clupeidarum opisthonomus, Osmerus jansseni, ?Synodidarum xenosus, Notolepis inconspectus, Myctophidarum biexcisus, Pseudocolliolus syltensis,Trisopterus angustus, Morone rectidorsalis, Sciaenidarum beseli, Lycodes lobatus, Trigloporus boschi , ?Sebastes fitchi and Lepidorhombus klockenhoffi, are given. One new species. Boreogadus similis, is described from the Lower Pliocene Kattendijk Sands of the Antwerp area (Belgium). One species of the Pliocene of Antwerp, Oncocottus asper, now is iden.tified as Enchelyopus.**
**The otolith faunas from Sylt are strongly dominated by the Gadidae and clearly show their own character; nevertheless they exhibit a much closer relationshlp with older Late Miocene faunas and even with Middle Miocene faunas than with the Pliocene to recent ones which are known from the North Sea Basin. The Syltian clays were formed in a quiet, open marine environment not very close to the coast, probably at depths between 50 and 100 m.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2020-01-19 **Last updated:** 2020-01-21
Squalicorax benguerirensis nov. sp.

* Taxonomy
* References

**1 -** **Cappetta, H., Adnet, S., Akkrim, D. & Amalik, Mohammed, 2014 - New Squalicorax species (Neoselachii: Lamniformes) from the Lower Maastrichtian of Ganntour phosphate deposit, Morocco**
***Palaeovertebrata*, 38 (2): 1–13** ; **3-5**:**3A-J**

**Copyright © JPP-Journals Wikia, 2014-2022****Created :** 2017-12-09 **Last updated:** 2018-04-27
Fossil sharks from Jamaica

<tabber>Description=

**Jamaican fossil fishes are rare and few nominal taxa have been recognised. To these can now be added *Carcharias* sp. (Eocene), *Carcharodon megalodon* ? L. Agassiz (late Cenozoic) and *Carcharodon* sp. (possibly Eocene), all identified from specimens in the Geology Museum, University of the West Indies, Jamaica.**
Fish otoliths from the Paleocene of Denmark

* Description
* Abstract
* Described species (22)
* New species (22)
* References (119)

**Both stages have previously been poorly known for otoliths in the North Sea Basin, and are described from only two previous publications, i.e. Koken in 1885 from the Selandian of Copenhagen and Roedel in 1930 who described otoliths from erratic ice age boulders in north-east Germany. The original material of both workers has been revised in this bulletin.Otoliths are well known elsewhere in the North Sea Basin since Upper Paleocene (Thanetian) times and are described from the London Basin and from Belgium. Palaeographic, palaeoecological and biostratigraphic implications of the otolith findings in the Paleocene of the North Sea Basin are discussed.**
**Two new genera and 23 new species are introduced and described. The new taxa are:*Genartina hauniensis* n. sp., genus Anguillidarum semisphaeroides n. sp., *Conger illaesus* n. sp., *Rhechias angulosus* n. sp., genus Clupeidarum rectiventralis n. sp., genus Salmonidarum acutirostratus n. sp., *Protargentinolithus procerus* n. sp., *Argentina longistrostris* n. sp., *Aulopus tortus* n. sp., genus Myctophidarum schnetleri n. sp., genus ?Percopsiformorum enigmaticus n. sp., *Palaeogadus sinangulatus* n. sp., *Molvia palaeomorpha* n. sp., *Protocolliolus amorphus* n. sp., *Coryphaenoides amager* n. sp., *Hymenocephalus rosenkrantzi* n. sp., genus Bythitidarm rasmussenae n. sp., genus Veliferidarum harderi n. sp., genus Zeiformorum janni n. sp., *Centroberyx fragilis* n. sp., *Scorpaena corallophilus* n. sp., genus Gempylidarum merus n. sp. and *Ostracion pergravis* n. sp.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-02-29 **Last updated:** 2020-01-14
Middle Miocene (Badenian) gastropods from Korytnica, Poland. Part V Addenda et Corrigenda ad Prosobranchia

* Description
* Abstract
* Described species ( )

**Five species are established as new: *Cocculina (Dallia) unica* sp.nov., *Turritella (Peyrotia) circumcisa* sp.nov., *Caecum korytnicense* sp.nov., *Morula valdemari* sp.nov., and *Ocinebrina recognita* sp.nov.**
**A new name, *Megalomphalus palazzii* nom.nov. is proposed for *Narica depressa* BOETTGER, 1907 [=*Megalomphalus depressus* (BOETTGER, 1907)], which is a homonym of *Megalomphalus depressus* (SEGUENZA, 1876).**

**Copyright © JPP-Journals Wikia, 2014-2022**
First Record of Soft-Shelled Turtles (Cryptodira, Trionychidae) from the Late Cretaceous of Europe

**1** **2** **3** ****4**** **5** **6** **7** **8** **9** **10** **11** **12** **13** **14** **15** **16** **17** **18** **19** **20** **21** **22** **23**

* Description
* Abstract
* Described species ( )
* References (60)

**Fossil soft-shelled turtles (Trionychidae) have so far been recognized in all continents except Antarctica, based largely on remains preserving their diagnostic sculptured shell bones. The origin of the group is generally assumed to be in the Early Cretaceous of Asia, whereas they first appear in North America and Europe during the Late Cretaceous and Paleocene, respectively. Here we describe the first record of an indeterminate trionychid from the late early Campanian from southern Sweden, a part of the paleobiogeographically isolated Fenno-Scandian Shield, thus extending the stratigraphic record of the group in Europe back about 15 Ma into the Late Cretaceous. Our finding provides evidence against the currently favored dispersal scenario in which trionychid turtles are interpreted to have come to Europe first during the Paleocene either directly from North America or via Asia. The described indeterminate trionychid possibly represents a relic of a pre-Cretaceous endemic radiation of North European trionychids living mainly on the Fenno-Skandian Shield or it may indicate a potential lower latitude dispersal route of trionychids from Asia to North America via Europe during the Late Cretaceous.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-03-08 **Last updated:** 2021-12-28
Fossil lanternfish otoliths of California, with notes on fossil Myctophidae of North America

* Description
* Abstract
* Described species (22)
* New species ( )
* References (20)

**Otoliths (sagitttae) from 30 species of lamternfishes (Myctophidae) are known from the North American Cenozoic: 15 from Plio-Pleistocene (California), 13 from Miocene (7 California: 5 Veracrus, Mexico; 1 Jamaica),and 2 from Eocene (California). The high incidence of species from California deposits, appears to be a reflection of the proximity of the shoreline to preferred myctophidae habitat (deep water), rather than a more abundant fauna, but both factors could be involved.**

**In addition to the species known from their otoliths, skeletal remains (imprints) of seven kinds of laternfishes have been found in Miocene diatomites of Southern California.Otoliths in some of these imprints make it possible to compare them with fossil myctophid sagittae that are unaccompanied by skeletal remains.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2017-01-29 **Last updated:** 2018-05-31
List Authors-G

A B C D E F **G** H I J K L M N O P Q R S T U V W Y Z All

1. - **Gutiérrez‎, G.** **(0)**
2. - **Gaetani‎, Maurizio** **(0)**
3. - **Gajdzik‎, Krzysztof‎** **(0)**
4. - **Gao‎‎, Shangyu‎** **(0)**
5. - **Ghirardelli, L. P.‎** **(0)**
6. - **Gibert‎, J. M. de‎** **(1)**
7. - **Gołębiowska‎‎, Bożena** **(0)**

A B C D E F **G** H I J K L M N O P Q R S T U V W Y Z All

**Copyright © JPP-Journals Wikia, 2014-2022**
Sur les Poissons fossiles de l'Eocène moyen d'Egypte

**1** **2** **3** **4** **5** **6** **7** **8** **9** **10** **11** **12** **13** **14** **15** **16** **17** **18** **19** **20** **21** **22** **23** **24** **25** **26** **27** **28** **29** **30** **31** **32** **33** **34** **35** **36** **37** **38** **39** **40** **41** **42** **43** **44** **45** **46** **47** **48** **49** **50** **51** **52** **53** **54** **55** **56** **57** **58** **59** **60** **61** **62** **63** **64** **65** **66** **67** **68** **69** **70** **71** **72** **73** **74** **75** **76** **77** **78** **79** **80** **81** **82** **83** **84** **85** **86** **87** **88** **89** **90** ****91**** **92** **93** **94** **95** **96** **97** **98** **99** **100** **101** **102** **103** **104** **105** **106** **107** **108** **109** **110** **111** **112** **113** **114** **115**

Described species

References
Review of the enigmatic Eocene shark genus Xiphodolamia (Chondrichthyes, Lamniformes) and description of a new species recovered from Angola, Iran and Jordan

* Description
* Abstract
* Described species (1)
* New species (1)
* References (66)

**Little is known about the extinct Xiphodolamia, a peculiar lamnid shark which inhabited the Eocene seas. The reexamination of a large set of fossilized teeth specimens from the Ypresian of Kazakhstan has enabled the reconstitution of the tooth series of this enigmatic taxa of lamnid shark. Five distinct tooth morphologies seem to occur in X. ensis Leidy [Leidy, J., 1877. Description of vertebrate remains, chiefly from the phosphate beds of South Carolina. Journal of the Academy of Natural Sciences of Philadelphia 8, 209-261] species revealing a weak ontogenetic variation. Such specific variation in tooth shape means that the other described species may be their junior synonyms. Dental morphology perfectly conforms with a Lamniforme but does not prove the current attribution to the Lamnidae family due to some inconsistent dental features observed, such as the presence of symphysial teeth. This genus could be regarded as an old lineage branched from the stem group of Lamnidae, close to the Isuroids sharks. Several *Xiphodolamia* teeth, originating both from old collections and new acquisitions, are reported and illustrated in order to provide information about a new species described here: *Xiphodolamia serrata* nov. sp. This species, currently limited to deposits in Angola, Jordan and Iran and dated at the Late Eocene, is easily distinguishable from the Early-Middle Eocene material belonging to the genus by the presence of serrated cutting edges. Adding to the type species considered here as the only valid taxa during the Early-Middle Eocene period, the temporal range of this genus extends to the Late Eocene, thus setting its upper stratigraphic limit prior to its disappearance as enigmatic as its appearance in the Early Eocene was.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-03-25 **Last updated:** 2018-07-10
Experiment

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* 1960-1969

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* 1970
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Les Étages et les Faunes du Bassin Tertiaire du Piémont

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Mollusques pleistocènes de la Côte française des Somalis, recueillis par E. Aubert de la Rüe

* Description
* Abstract
* Described species

Maastrichtian of the Benguérir phosphate open mine, Ganntour deposit, Morocco. The species S. benguerirensis nov. sp. was
classically assigned to S. yangaensis by Arambourg (1952) and has been also recognized in coeval deposits from eastern USA to
Mid-East. The species S. microserratus nov. sp. corresponds to the lateral teeth of S. kaupi as reported by Arambourg (1952) and
which is now referred to S. bassanii. The comparison of these two new species with other anacoracids, known from Morocco or
elsewhere, allows the great taxonomic and ecological diversities of this family during the Cretaceous to be highlighted

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**Copyright © JPP-Journals Wikia, 2014-2022**
**Last updated:** 2018-03-09
First Record of Kimbetohia campi (Mammalia, Multituberculata) from the Paleocene Part of the North Horn Formation, Utah

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* Description
* Abstract
* Described species (0)
* New species (0)
* References (0)

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**Created :** 2017-11-04 **Last updated:** 2021-12-29
New information on the Devonian shark Mcmurdodus, based on material from western Queensland, Australia

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* Description
* abstract
* Described species ( )
* New species ( )
* References (32)

discernible in *Mcmurdodus* teeth, but a parallel-fibred layer is possibly present. Prismatic calcified cartilage, presumed to be fromM. whitei, appears identical to that of all elasmobranchs. Scales and spines and distinctive ringlike elements occur in the same horizon, the latter comparable with elements that encircle the lateral line in Echinorhinus, and which are found in no other Recent elasmobranchs**.**

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**Created :** 2018-07-09 **Last updated:** 2018-07-11