recursal/Fanatic-Fandom huggingface dataset:
A New Archosaur (Diapsida, Archosauriformes) from the Marine Triassic of China

**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 (0)
* New species (0)
* References (0)

**A new Middle Triassic archosaur, *Diandongosuchus fuyuanensis*, gen. et sp. nov., is described on the basis of a skeleton from the Zhuganpo Member (Ladinian) of the Falang Formation, eastern Yunnan Province, China. It is primarily characterized by the nasal process of the premaxilla extending posteriorly well beyond the external naris, the super-sized coracoid foramen laterally bordered by the scapula, the ischium with a strongly expanded medial portion anteroposteriorly longer than the proximodistal height of the bone, and anteriorly notched cervical osteoderms. *D. fuyuanensis* is a pseudosuchian on the basis of the crocodile-normal tarsal joint and other features, such as the distal end of the ulna in posterolateral view squared off, osteoderms with a distinct anterior process, the presacral vertebrae dorsally covered by more than one osteoderm, dorsal osteoderm alignment dorsal to presacrals 10–24 staggered, the pubis-ischium contact reduced to a thin proximal contact, and the medial contact of the ischia extensive but the dorsal margins separate. It is from a marine deposit but shows few morphological adaptations of the postcranial skeleton for a semiaquatic way of life when compared with *Qianosuchus* from the Anisian limestone of the same area. A phylogenetic analysis derived from an existing data matrix suggests that the new archosaur occupies the basal-most position in Poposauroidea and further confirms the poposauroid status of *Qianosuchus*. On the basis of current information, the discovery of *Diandongosuchus* does not firmly underscore the affinity of the semiterrestrial vertebrate faunas between the eastern and western regions along the northern coastline of the Tethys.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2017-11-04 **Last updated:** 2021-12-28
Chondrichthyans from the Pennsylvanian (Desmoinesian) Naco Formation of central Arizona

* Description
* abstract
* Described species ( )
* New species ( )
* References (81)

**This fauna is similar to others in New Mexico, Colorado, and Ohio and constitutes a western extension of such faunas in North America. In addition, the presence of *Deltodus sublaevis* and *Lagarodus angustus* documents a range extension from a known European distribution, reinforcing the cosmopolitan nature of chondrichthyan faunas at this time.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-07-11 **Last updated:** 2018-07-12
1551 Vertebrate Paleontology Reference List

**1541 1542 1543 1544 1545 1546 1547 1548 1549 1550 1552 1553 1554 1555 1556 1557 1558 1559 1560 1561**

* G-1

**1. Gesner, Conrad (1551) - *Historiae animalium lib. I.De quadrupedibus viviparis*.
Fol., Zurich. 38 + 1104 + 9 pp., figs.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-04-18 **Last updated:** 2018-06-03
A Nearly Complete Skeleton of Ernanodon (Mammalia, Palaeanodonta) from Mongolia: Morphofunctional Analysis

****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 (1)
* References (60)

***Ernanodon*, one of the most enigmatic Asian fossil mammals, was previously known by a single specimen from the late Paleocene (Nongshanian) of China. Here we document the first record of *Ernanodon* from Mongolia, represented by a nearly complete skeleton from the late Paleocene (Gashatan) of the Naran Bulak locality. The new material provides an opportunity to understand the lifestyle and habits of this rare mammal and reevaluate the arguments used to establish the phylogenetic relationships of *Ernanodon*. Functional analysis indicates that *Ernanodon* had very strong forelimbs with large claws and used its forelimbs for scratch-digging. Character analysis reveals numerous similarities in postcranial anatomy between *Ernanodon* and Palaeanodonta. Phylogenetic analysis supports inclusion of *Ernanodon* in the order Palaeanodonta and suggests that Palaeanodonta and Pholidota are sister groups.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-03-07 **Last updated:** 2021-12-28
Early Frasnian sharks from central Iran

**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 (18)

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-07-10 **Last updated:** 2018-07-10
1906 Vertebrate Paleontology Reference List

**1896 1897 1898 1899 1900 1901 1902 1903 1904 1905 1907 1908 1909 1910 1911 1912 1913 1914 1915 1916**

* A-L
* M-Z

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

**1. **Abel, Othenio** (1906) - Die Milchmolaren der Sirenen.
*Neues Jarhb. Min. Geol Pal, Abh.*, 1906(2):50-60.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-24 **Last updated:** 2018-08-07
Тихая ночь(Фан)

## **Пролог**

В широкой, тёмной пещере лежала чёрная, старая кошка. Её ярко – янтарные глаза сверкали в ночных сумерках.

- Медовая Звезда! – густую, ночную тишину прорезал требовательный, громкий голос.

- Это ты Льдинохвост? – Медовая Звезда выгнула спину и вышла из пещеры к глашатаю.

Остановившись возле белого кота, она села на холодную землю. Вдруг глашатай кинулся на старую кошку и вцепился ей в горло. Тонкими задними лапами Медовая Звезда старалась поранить не защищённый живот Льднохвоста, вцепиться в его плечо и одержать победу, но силы покидали её старое измученное тело.

В это время белоснежный кот стал прочёсывать её бока длинными, изогнутыми
когтями и оскалил клыки.

-Зачем? – единственное слова которое вырвалось из Медовой Звезды, опалив шерсть Льдинохвоста холодным дыханием смерти, прежде, чем глашатай вцепился ей в горло.

Медовой Звезде показалось, что огромная чёрная, как самая непроглядная ночь лавина накрыла её с головой.

Янтарные глаза предводительницы потухли, уставившись куда –то сквозь Льдинохвоста.

Сквозь переплетённые ветви ежевики и папоротника можно было видеть светло
– бурую королеву с белой мордочкой. Кошка вылизывалась рядом с ещё одной серой
королевой. Подруги о чём – то весело болтали, как вдруг морда бурой королевы мгновенно
скривилась, и она зажмурилась от боли.

- Я скажу за Ручьём! – серая королева встала со своего гнёздышка и оглянулась
на два маленьких комочка, спящих на мягкой подстилке.

- Я пригляжу за ними, Блёстка! – бурая королева поймала тревожный взгляд
кошки и понимающе уставилась на неё.

- Спасибо! – Блёстка кивнула королеве и вышла из детской.

- У тебя две девочки, Цветогривка! – сказал маленький, старый рыжий кот
осматривая двух крошечных котят жадно сосущих молоко, - Ты можешь не говорить
нам кто их отец.

- Как ты их назовешь? – спросила Блёстка вопросительно глядя на подругу.

- Пожалуй… - Цветогривка задумалась и посмотрела на шубки дочек.  Один комок был тёмно – бурый, а другой
чёрный, - Полосочка – она погладила хвостом бурую малышку, и посмотрела на
маленькую чёрную кошечку - И Чернушка.

Вот и славно! – Ручей провёл хвостом по малышкам и вышел из детской.
Description of Karaganops n. gen. perratus (Daniltshenko 1970) with otoliths in situ, an endemic Karaganian (Middle Miocene) herring (Clupeidae) in the Eastern Paratethys

* Description
* Abstract
* Described species
* References (24)

**The following fishes have been identified from the semimarine Karaganian deposits: silversides—*Atherina prima* Switchenska 1959, mullets—*Mugil karaganicus* Switchenska 1973, lefteye flounders—*Arnoglossus ovalis* Switchenska 1981, as well as the endemic euryhaline herring *Karaganops perratus* (Daniltshenko 1970) n. gen. Articulated skeletons of this clupeid species were described from the Middle Miocene deposits of the Tambov region by P. G. Daniltshenko as *Sardinella perrata*. In addition to Tambov, further specimens were described from locations in the Caucasus.**
**In the original description of *S. perrata*, Daniltshenko clearly separated these two forms. He noted differences in the number of vertebrae and the number of fin rays as distinctive features, but without further specifications. Later in the article the author pointed out that ‘‘… Karaganian representatives of *Sardinella* in the Caucasus form a separate species, the description of which… will be devoted to a special work’’ (Daniltshenko and Iosifova 1970, p. 165). However, such paper has never been published.**
**We compared material from both locations (the Tambov material from literature, since Daniltshenko’s original collection could not be located) and found that there are no obvious differences between specimens from both regions other than small differences in the body measurements and the number of vertebrae. Given the high degree of variability of these characters in clupeid fishes, we conclude that distinction of two separate species does not appear to be warranted with the data currently available.**

**Copyright © JPP-Journals Wikia, 2014-2022**
1554 Vertebrate Paleontology Reference List

**1544 1545 1546 1547 1548 1549 1550 1551 1552 1553 1555 1556 1557 1558 1559 1560 1561 1562 1563 1564**

* B-1
* G-1

**1. Boccacio, Giovanni (1554) - *I quindici libri sopra la origine, et discendenza di tutti gli Dei de' gentili*.
8 (degree), Venice. xiv + 263 pp.; fol., 32 pp.**

**1. Gesner, Conrad (1554) - *Appendix Historiae quadrupedum viviparorum et oviparorum*.
Fol., Zurich. 27 pp., figs.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-04-18 **Last updated:** 2018-06-03
2003 Vertebrate Paleontology Reference List

**1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013**

* A-L
* M-Z

* A-0
* B-0
* C-0
* D-0
* E-0
* F-0
* G-0
* H-0
* I-0
* J-0
* K-0
* L-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-20 **Last updated:** 2018-08-02
A comparative morphological study of the Recent otoliths of the genera Diaphus, Idiolychnus and Lobianchia (Myctophidae)

* Description
* Abstract
* Described species (0)
* New species (0)
* References (38)

**The unaccounted species are either represented only by their respective unique holotypes or specimens were unavailable for investigation or did not yield preserved otoliths. Sixteen otolith characters are defined for the otoliths of these genera in order to facilitate incorporation of otolith data for future phylogenetic analysis of Diaphini.**
**The morphology of *Diaphus* otoliths is diverse and can be used for definition of otolith groups and subgroups which are combined in 3 major units as follows: unit 1 – *Diaphus theta*, *Diaphus termophilus* and *Diaphus signatus* otolith groups; unit 2 – *Diaphus splendidus* otolith group; unit 3 – *Diaphus garmani*, *Diaphus fragilis*, *Diaphus adenomus*, *Diaphus effulgens*, *Diaphus perspicillatus* and *Diaphus metopoclampus* otolith groups. Prime characters used to distinguish otolith groups and units are: curvature of inner and outer faces, shape of postdorsal rim, particularly the presence, shape and position of the postdorsal angle and the postdorsal depression which follows the postdorsal angle, length of rostrum, relative proportions of ostium to cauda and number of denticles on the ventral rim.However, certain species exhibit a very generalized otolith morphology that allows only a tentative allocation with any otolith group.The findings of the grouping of the otolith morphologies are compared to the groupings published based on ‘whole fish’ investigations, primarily by the pattern of the head luminous organ, and show a reasonable degree of concordance between them in several of the groups, but also instances of conflicting allocations.**
**The otoliths of the two genera *Idiolychnus* and *Lobianchia* show a large degree of similarity with otoliths of *Diaphus*, to such an extent even that they could be integrated into different otolith groups of that genus from an ‘otolith only’ perspective. The otoliths of the two species in *Lobianchia* in fact are so divergent that separation of *L. dofleini* to a separate genus would be justifiable.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-07-13 **Last updated:** 2018-07-29
1590 Vertebrate Paleontology Reference List

**1580 1581 1582 1583 1584 1585 1586 1587 1588 1589 1591 1592 1593 1594 1595 1596 1597 1598 1599 1601**

* A-1

**1. Albinus, Petrus (1590) - *Meissnische Land und Berg-Chronica*.
Dresden, 2 vols. x + 449 pp. (1589); vi + 204 pp. (1590).**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-06-03 **Last updated:** 2018-06-18
A New Genus and Species of Boxfish (Tetraodontiformes: Ostraciidae) from the Oligocene of Moravia, the Second Fossil Representative of the Family

* Description
* Abstract
* Described species ( )
* New species (1)
* References (48)

**The new species is a typical member of the in-shore benthic Ostraciidae, but the other fishes with which it is associated in the Menilitic Formation are nearly all more off-shore mesopelagic species of Myctophidae and Gonostomatidae. To account for this, we propose that the new species represents the oceanic, pelagic, pre-settlement stage of this genus, as in the Recent Lactoria, some species of which, especially L. diaphana, remain pelagic to sizes of over 100 mm SL and can be sexually mature while pelagic before settling into their conclusive benthic state.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-01-03 **Last updated:** 2021-12-30
1835 Vertebrate Paleontology Reference List

**1825 1826 1827 1828 1829 1830 1831 1832 1833 1834 1836 1837 1838 1839 1840 1841 1842 1843 1844 1845**

* A-L
* M-Z

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

**1. **Agassiz, Louis** (1835) - On the fossil fishes of Scotland.
*Report Brit. Assoc. Adv. Sci.*, 4th meeting, Edinburgh, 1834, pp. 646-647**

**2. American Journal of Science (1835) - Vertebral bone of a mastodon.
*Amer. Jour. Sci*.,xxvii, pp. 165-166**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-24 **Last updated:** 2018-08-03
1579 Vertebrate Paleontology Reference List

**1569 1570 1571 1572 1573 1574 1575 1576 1577 1578 1580 1581 1582 1583 1584 1585 1586 1587 1588 1589**

* B-1
* F-1

**1. Balbinus, Bohuslav (1579) - *Miscellanea historica regni Bohemiae. Liber I qui historiam naturalem Bohemiae complectitur*.
Fol., Prague, vii + 181 + xxiii pp.**

**1. Fazellus, Thomas (1579) - *Rerum sicularum scriptores ex recentioribus praecipui, in unum corpus nunc primun congesti, diligentique recognitione plurimis in locis emendati*.
Fol., Frankfurt am Main. vii + 705 pp. + index.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-28 **Last updated:** 2018-06-03
1572 Vertebrate Paleontology Reference List

**1562 1563 1564 1565 1566 1567 1568 1569 1570 1571 1573 1574 1575 1576 1577 1578 1579 1580 1581 1582**

* G-1

**1. Glycas, Michael (1572) - *Annales, qui lectori praeter alia cogniti iucunda et utilia Byzantinam historiam universam exhibent.* Transl. into Latin by lo.
Lewenclaius.Basel. 512 pp. + index.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-28 **Last updated:** 2018-06-03
1851 Vertebrate Paleontology Reference List

**1841 1842 1843 1844 1845 1846 1847 1848 1849 1850 1852 1853 1854 1855 1856 1857 1858 1859 1860 1861**

* A-L
* M-Z

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

**1. **Agassiz, Louis** (1851) - [Announcement of the finding of the head of a walrus on New Jersey shore.]
*Proc. Amer. Assoc. Adv. Sci.*, 4th meeting, New Haven, 1850, p. 252**

**2. **Agassiz, Louis** (1851) - Report on the vertebrate fossils exhibited to the Association (abstract).
*Proc. Amer. Assoc. Adv. Sci.,* 5th meeting, Washington, D. C., 1851, pp. 178-180**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-20 **Last updated:** 2018-08-03
1850 Vertebrate Paleontology Reference List

**1840 1841 1842 1843 1844 1845 1846 1847 1848 1849 1851 1852 1853 1854 1855 1856 1857 1858 1859 1860**

* A-L
* M-Z

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

**1. **Agassiz, Louis** (1850) - On the fossil remains of an elephant found in Vermont.
*Proc. Amer. Assoc. Adv. Sci.*, 2d meeting, Cambridge, Mass., pp. 100-101**

**2. **Agassiz, Louis** (1850) - Remarks on finding femur of Atlantochelys.
*Proc. Nat. Hist. Soc. Boston*, III, p. 351**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-20 **Last updated:** 2018-08-03
Diatom, phytolith, and pollen records from a 10Be/9Be dated lacustrine succession in the Chad basin: Insight on the Miocene–Pliocene paleoenvironmental changes in Central Africa.

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

**Well-preserved diatom assemblages first occurred at 4.7 ± 0.1 Ma and were dominated by the freshwater planktonic genera Aulacoseira and Stephanodiscus until the end of the Pliocene. This supports the recurrence of lacustrine conditions at Bol during all the Pliocene. The presence of pelite and argillaceous deposits in the core before 4.7 ± 0.1 Ma, however, suggests that the lake settled earlier, at least since 6.3 ± 0.1 Ma. The abundance of Afromontane pollen taxa at 4.2 ± 0.1 Ma and the occurrence of trapeziform polylobate phytoliths throughout the sequence suggest significant vegetation inputs from the southern highlands, while the importance of kaolinite in the clay sediments indicates a water supply predominantly from the south during the Pliocene.**
**Phytolith assemblages are all dominated by lobate grass silica short cells and by blocky and elongate types, which attest to the presence of herbaceous-dominated vegetation around Bol and/or in the southern drainage basin during the Pliocene. This result is also supported by the pollen assemblage described at 4.2 ± 0.1 Ma, which shows highest affinity for the savanna biome. Moreover, low values for the Xerophytic grass phytolith index indicate the presence of humid-loving (mesophytic and aquatic) grass communities in this vegetation.**
**At last, significant variations in the abundance of blocky and elongate phytoliths are indicative of local alternations of fully lacustrine and marshy conditions at Bol. Particularly between 3.6 and 2.7 Ma, the abundance of silicified bulliform cells combined with the absence of diatoms support a significant lacustrine reduction at Bol favoring the increasing of local marshy vegetation.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-03-26 **Last updated:** 2021-12-31
A new Late Ordovician erratic anthaspidellid sponge (Porifera) originating from Baltica

****1**** **2**

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

**The new anthaspidellid taxon Brevaspidella dispersa is erected for specimens recovered from the Late Ordovician sponge assemblages of the island of Gotland, Sweden and the Dutch-German border region. In the latter area, they are collected from Early Pleistocene fluvial deposits of the Baltic River System, whereas those from Gotland are part of Late Pleistocene glacial or fluvio-glacial deposits. The provenance of both assemblages is uncertain, but they probably originated from an Ordovician basin in the northern Baltic Sea or the Bothnian Gulf, west of Finland. As yet, *Brevaspidella dispersa* gen. et sp. nov. is restricted to the Gotland-German-Dutch sponge association and has not been found in the assemblage of nearly-coeval ‘lavender-blue cherts’ and ‘blue sponges’. The new taxon is closely related to the genus Anthaspidella, but differs in the aquiferous system and in having a well developed concentrically wrinkled dermal layer.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2017-12-11 **Last updated:** 2018-06-09
1569 Vertebrate Paleontology Reference List

**1559 1560 1561 1562 1563 1564 1565 1566 1567 1568 1570 1571 1572 1573 1574 1575 1576 1577 1578 1579**

* B-1

**1. Becanus, Ioan Goropius (1569) - *Origines antwerpianae, sive cimmeriorum Becceselana*.
Fol., Antwerp, xxx + 1058 pp.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-28 **Last updated:** 2018-06-03
A New Extinct Inioid (Cetacea, Odontoceti) from the Upper Miocene Senhata Formation, Chiba, Central Japan: The First Record of Inioidea from the North Pacific Ocean

**1** **2** ****3**** **4** **5** **6** **7** **8**

* Description
* Abstract
* Described species ( )
* New species ( )
* References (71)

**Inioidea, which consists of Iniidae and Pontoporiidae, includes only four extant species, all of which occur in South America. Inioids were, however, more diversified and widely distributed in the past, starting from the late middle Miocene, as recorded from the eastern Pacific, North and South Atlantic, North Sea and the riverine systems of South America. In this paper, the author describes a new extinct inioid, Awadelphis hirayamai gen. et sp. nov. (WU SILS G 408), from the uppermost Miocene Senhata Formation (6.3–5.7 Ma) of Chiba, central Japan. Morphological cladistic analysis supports placement of this new taxon within the Inioidea. The new species is characterized by a right premaxillary eminence with a pronounced overhang on the right maxilla and a short zygomatic process of the squamosal. This is the first fossil record of an inioid not only from Japan but also from the North Pacific. The discovery of this new taxon considerably extends the paleobiogeographic range of inioids, and indicates that inioids co-occurred with other small odontocetes of the western North Pacific, where delphinoids dominated. The new species is also the first valid occurrence of a small odontocete from tropical—subtropical climates of the late Miocene in the western North Pacific.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2017-11-07 **Last updated:** 2021-12-29
1998 Vertebrate Paleontology Reference List

**1988 1989 1990 1991 1992 1993 1994 1995 1996 1997 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008**

* A-L
* M-Z

* A-0
* B-0
* C-0
* D-0
* E-0
* F-0
* G-0
* H-0
* I-0
* J-0
* K-0
* L-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-06-30 **Last updated:** 2018-06-30
1847 Vertebrate Paleontology Reference List

**1837 1838 1839 1840 1841 1842 1843 1844 1845 1846 1848 1849 1850 1851 1852 1853 1854 1855 1856 1857**

* A-L
* M-Z

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

**1. American Journal of Science (1847) - Harlanus, a new genus of fossil pachyderms.
*Amer. Jorn. Sci.*, (2), III, p. 125.**

**2. American Journal of Science (1847) - Ornithichnites.
*Amer. Jorn. Sci.*, (2), III, p. 276**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-20 **Last updated:** 2018-08-03
1563 Vertebrate Paleontology Reference List

**1553 1554 1555 1556 1557 1558 1559 1560 1561 1562 1564 1565 1566 1567 1568 1569 1570 1571 1572 1573**

* G-1

**1. Gesner, Conrad (1563) - *Thierbuch, das ist ein kurtze Bschreybung aller vierfüssigen Thieren/ so auff der Erde und in Wassern wonend/ sampt jrer Waren Conterfactur/ ... Yetzunder durch D. Cunrat Forer ... in das teutsch gebracht*.
Zurich. 4 + clxiii pp., illus.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-28 **Last updated:** 2018-06-03
2006 Vertebrate Paleontology Reference List

**1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2007 2008 2009 2010 2011 2012 2013 2014 2015 2016**

* A-L
* M-Z

* A-0
* B-0
* C-0
* D-0
* E-0
* F-0
* G-0
* H-0
* I-0
* J-0
* K-0
* L-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-20 **Last updated:** 2018-08-02
1852 Vertebrate Paleontology Reference List

**1842 1843 1844 1845 1846 1847 1848 1849 1850 1851 1853 1854 1855 1856 1857 1858 1859 1860 1861 1862**

* A-L
* M-Z

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

**1. American Journal of Science (1852) - The Mastodon giganteus of North America, by John C. Warren, M. D.
*Amer. Jour. Sci.*, (2), XIV, p. 454**

**2. American Journal of Science (1852) - On a fossil saurian of the New Red sandstone formation of Pennsylvania, with some account of that formation, etc., by Isaac Lea.
*Amer. Jour. Sci.*, (2), XIV, p. 451**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-20 **Last updated:** 2018-08-03
1580 Vertebrate Paleontology Reference List

**1570 1571 1572 1573 1574 1575 1576 1577 1578 1579 1581 1582 1583 1584 1585 1586 1587 1588 1589 1590**

* C-1
* P-1

**1. Cassanio, Jean (1580) - *De gigantibus eorumque reliquiis, atque iis, quae ante annos aliquot nostra aetate in Gallia repertae sunt*.
Basel.**

**1. Palissy, Bernard (1580) - *Discours admirables, de la nature des eaux et fontaines, tant naturelles qu'artificielles, des métaux, des sels and salines, des pierres, des terres, du feu and des emaux*.
Paris. 15 + 361 + 23 pp.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-28 **Last updated:** 2018-06-03
2004 Vertebrate Paleontology Reference List

**1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2005 2006 2007 2008 2009 2010 2011 2012 2013 2014**

* A-L
* M-Z

* A-0
* B-0
* C-0
* D-0
* E-0
* F-0
* G-0
* H-0
* I-0
* J-0
* K-0
* L-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-20 **Last updated:** 2018-08-02
2008 Vertebrate Paleontology Reference List

**1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2009 2010 2011 2012 2013 2014 2015 2016 2017 2018**

* A-L
* M-Z

* A-0
* B-0
* C-0
* D-0
* E-0
* F-0
* G-0
* H-0
* I-0
* J-0
* K-0
* L-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-20 **Last updated:** 2018-08-03
Долина Гейзеров (станция)

Период времени
 Обитатели

**Долина Гейзеров** — станция, располагающиеся в Северной Америке мелового периода. Появляется в одноимённой серии.

## Описание

Вокруг этой станции располагается хвойный лес. Есть множество гейзеров, выстреливающих в определённое время горячей водой. Сюда приезжают множество динозавров со всех концов мезозойской эры, чтобы посмотреть на гейзеры. Рядом располагаются горячие источники, в которых можно отдохнуть.
Evolutionary history of the devilrays(Chondrichthyes: Myliobatiformes) from fossil and morphological inference.

* Description
* Abstract
* Described species (12)
* New species (3)
* References (83)

**The exact affinities of the fossil teeth attributed to the devilrays (mobulids) are critical for resolving the debated origin of these giant pelagic rays amongst Myliobatiformes and the timing of their evolution toward planktivory. We performed the first detailed comparative description of teeth belonging to most of the living and fossil mobulids. Based on a survey of living devilrays, three dental morphologies are newly identified as cobblestone tooth plates, comb-like teeth, and peg-like teeth. In addition, all extinct mobulid species are reviewed with comments on their dentition, fossil record, and geographical distribution. As a result, three fossil mobulid taxa are newly described from the Late Eocene of south-west Morocco (*Argoubia barbei* gen. et sp. nov., *Oromobula dakhlaensis* gen. et sp. nov., and *Eoplinthicus underwoodi* sp. nov.). This has permitted the first assessment of the phylogenetic positions of extinct and extant species of mobulids, using cladistic analyses and a combined data set of nondental anatomical characters from the literature and the dental characters defined here. Our new results support the monophyly of mobulids including all living and most extinct species and indicate that mobulids are closely related o rhinopterids. They also indicate that there was a recent split within Mobulidae into the three tooth morphology groups that we describe in this paper. This work provides clues to the evolutionary history of this clade since the Early Eocene, including the gradual lack in tooth interlocking toward the filter-feeding strategy, whereas the preservation of cusped teeth without feeding function in modern filter-feeder mobulids is interpreted as a tool for precopulatory purposes.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-03-28 **Last updated:** 2018-06-02
A Late Santonian fish-fauna from the Eutaw Formation of Alabama reconstructed from otoliths

* Description
* Abstract
* Described species (18)
* New species (10)
* References (65)

**The otoliths described here from the Late Santonian of the Eutaw Formation of Alabama, represent one of the earliest association of teleost otoliths known from North America and it is remarkable for its good preservation and species diversity. They were collected by the late C.K. Lamber in 1969 from a road cut on the Hurtsboro-Marvyn highway south of Marvyn in Russell County, eastern Alabama. It contains 18 taxa based on sagittae otoliths, of which 14 are identifiable to the species level, 10 species are new to science and five new genera. The new otolith-based genera are: *Allogenartina* n. gen. (Stomiiformes family indet.), *Pseudotrichiurus* n. gen. (Aulopiformes family indet.), *Eutawichthys* n. gen. (Beryciformes family indet.), *Cowetaichthys* n. gen. (Polymixiidae) and *Vox* n. gen. (Teleostei family indet.); the new species are: *Elops eutawanus* n. sp., *Genartina cretacea* n. sp., *Allogenartina muscogeei* n. sp., *Pseudotrichiurus sagax* n. sp., *Apateodus? assisi* n. sp., *Eutawichthys compressus* n. sp., *Eutawichthys stringeri* n. sp., *Cowetaichthys alabamae* n. sp., *Cowetaichthys lamberi* n. sp. and *Vox thlotlo* n. sp. In addition, 8 different morphologies are recognized based on lapilli otoliths, which however cannot be identified to a distinct taxonomic level except for a species of the Ariidae. Two taxa can be related to otoliths recently recorded in situ, pertaining to the genera *Osmeroides* and *Apateodus*.**
**The otolith association bears much similarity with those of the Campanian to Maastrichtian of the USA described previously as indicated by the dominance of otoliths of the genera Eutawichthys and Osmeroides. Differences with those faunas are on the species level as well as in the accessory components. The abundance of otoliths of the albuliforms (Osmeroides), putative stomiiforms (*Allogenartina*), beryciform (*Eutawichthys*) and polymixiids (*Cowetaichthys*) characterizes a rather stable faunal composition through the entire Late Cretaceous of locations studied in the USA.**

**The conundrum of interpreting the systematic position of isolated Late Cretaceous otoliths is discussed and the findings are correlated with the rich fish fauna known from articulated skeletons of the coeval Niobrara Formation. We consider the taxonomic position of the majority of isolated otoliths to be more or less consistent with the skeletal findings, but there are also a few otolith morphologies, which do not seem to have a skeletal equivalent in the Niobrara Formation, e.g. in osteoglossiforms, clupeiforms, stomiiforms and Ariidae.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-06-07 **Last updated:** 2021-12-29
1848 Vertebrate Paleontology Reference List

**1838 1839 1840 1841 1842 1843 1844 1845 1846 1847 1849 1850 1851 1852 1853 1854 1855 1856 1857 1858**

* A-L
* M-Z

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

**1. **Agassiz, Louis** (1848) - [Letter to Dr. Gibbes regarding Dorudon.]
*Proc. Acad. Nat. Sci. Phila*., IV, p.4**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-20 **Last updated:** 2018-08-03
1837 Vertebrate Paleontology Reference List

**1827 1828 1829 1830 1831 1832 1833 1834 1835 1836 1838 1839 1840 1841 1842 1843 1844 1845 1846 1847**

* A-L
* M-Z

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

**1. Anonymous (1837) - Fossil remainsof the elephant, Elephas primigenius.
*Amer. Jour. Sci*.,xxxii, pp. 377-379**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-24 **Last updated:** 2018-08-03
El Género Isistius (Squalidae) en el Alto Guayacán.Formación Uscari (Mioceno Superior-Plioceno Inferior), Provincia de Limón, Costa Rica

Described species

References

ANTUNES, M.T. & JONET, S., 1970: Requins de l’Helvé-tien supérieur et du Tortonien de Lisbonne.- Rev. Fac.Cienc., Univ. Lisboa, 2. Ser. C (cienc. Natur), 16 (1):119-280.
CAPPETTA, H., 1970: Les sélaciens du Miocène de la regionde Montpellier. - Paleovertebrata, Mém. extraordinai-re 1970: 1-139.CAPPETTA, H., 1987: Handbook of paleoichthyology, Vol. 3BChondrichthyes II. Mesozoic and Cenozoic Elasmo-branchii. - Gustav Fischer Verlag, New York, 193 págs.
CAPPETTA, H., GRANIER, J. & LEDOUX, J.C., 1967:Deux faunes des Sélaciens du Miocene méditerranéende France et leur signification bathymétrique. - C.R.somm. Soc. géol. Fr., 7: 292-293.
CAPPETTA, H. & LEDOUX, J.C., 1970: Comparaison de lafaune ichthyologique miocene avec actuelle de Médi-terranée. - Journées icththyol., 21-23.- Rome,C.I.E.S.M.
CASIER, E., 1958: Contribution à l’étude des Poissons fossi-les des Antilles. - Mém. Suisses de Paléontolgie, 74:95 págs.
CASIER, E., 1966: Sur la faune ichthyologique de la Forma-ción de Bissex Hill et de la série océanique, de l’Ile dela Barbade, et sur l’âge de ces formations. - Eclogaegeologicae Helvetie, 59(1): 493-515.
COMPAGNO, L.J.V., 1984: FAO species catalogue. Vol. 4Sharks of the world. An annotaded and ilustrated ca-talogue of sharks species known to date. - FAO fish.Synop., 125(4), Part. 1: 1-249; Part. 2: 251-665.
GARRICK, J.A.F. & SPRINGER, S., 1964: Isistius plutodus,a new squaloid shark from the Gulf of Mexico. - Co-peia 1964, 4: 678-682.
GILLETTE, D.G., 1984: Amarine ichthyiofauna from theMiocene of Panamá, and tertiary caribbean faunalprovince. - En: MacFadden, B.J. (ed.): Origin andevolution of the Cenozoic vertebrate fauna of Midd-le America. - J. Vertebrate Paleontology, 4(2): 172-186.
KOZAREK, R.J. & ORR, W.N., 1980: Ichthyoliths, DeepSea Drilling Project Legs 51 through 53. - En: Init.Rep. DSDP, 51, 52, 53(2): 857-895.
LEDOUX, J.C., 1972: Les Squalidae (Euselachii) miocènesdes environs d’Avignon (Vaucluse).- DocumentsLab. Géol. Fac. Sci. Lyon, Notes et Mém., 52: 133-175.
LONGBOTTOM, A., 1979: Miocene shark’s teeth fromEcuador. - Bull. Brit. Mus. Natur. Hist. (Geol.), 32(1):57-70.
SERRALHEIRO, R., 1954: Contribução para o conhecimen-to da fauna ictiológica do miocéno marinho de Portu-gal Continental. - Rev. Faculd. Ciênc. de Lisboa, C,4(1): 39-119.
STRASBURG, D.W., 1963: The diet and dentition of Isistiusbrasiliensis, with remarks on tooth replacement in ot-her sharks. - Copeia, 1963, 1: 33-40.
ZBYSZEWSKI, G. & MOITINHO D’ALMEIDA, F., 1950:Os peixes miocénicos portugueses. - Comn. Serv.Geol. de Portugal, XXI: 309-412
2011 Vertebrate Paleontology Reference List

**2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 2012 2013 2014 2015 2016 2017 2018 2019 2020 2021**

* A-L
* M-Z

* A-0
* B-0
* C-0
* D-0
* E-0
* F-0
* G-0
* H-0
* I-0
* J-0
* K-0
* L-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-20 **Last updated:** 2018-08-03
A new shark and ray fauna from the Middle Miocene of Mazan, Vaucluse (southern France) and its importance in interpreting the paleoenvironment of marine deposits in the southern Rhodanian Basin

* Description
* Abstract
* Described species (33)
* New species (0)
* References (90)

**Recent paleontological excavations of the Middle Miocene sandstones (top of the ‘‘Schlier’’ facies) near Mazan, Vaucluse (southern France) uncovered a rich selachian teeth assemblage including 34 shark and ray species. This great diversity of selachian taxa provides new information about the palaeoenvironmental settings of some Middle Miocene deposits in the southern Rhodanian basin. For instance, the co-occurrence of some deepwater Squaliformes and Rajidae with numerous Carcharhiniformes and Myliobatiformes, usually inhabiting the continental shelf, suggests a deepwater deposit inshore, as adjacent to a submarine canyon area.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-06-10 **Last updated:** 2021-12-31
1883 Vertebrate Paleontology Reference List

**1873 1874 1875 1876 1877 1878 1879 1880 1881 1882 1884 1885 1886 1887 1888 1889 1890 1891 1892 1893**

* A-L
* M-Z

* A-5
* B-0
* C-0
* D-0
* E-0
* F-0
* G-0
* H-0
* I-0
* J-0
* K-0
* L-0

**1. **Ameghino, Florentino** (1883) - Mamíferos y aves fósiles argentinos. Especies nuevas, adiciones y correcciones.
*Crónica Científica de Barcelona*, 14:340-348, 380-383.**

**2. **Ameghino, Florentino** (1883) - Sobre la necesidad de borrar el género Schistopleurum y sobre la clasificación y sinonimia de los gliptodontes en general.
*Boletín de la Academia Nacional de Ciencias, Córdoba*,. 5:1-34.**

**3. **Ameghino, Florentino** (1883) - Sobre una colección de mamíferos fósiles del piso mesopotámico de la Formación patagónica, recogidos en las barrancas del Paraná por el profesor Pedro Scalabrini.
*Boletín de la Academia Nacional de Ciencias*, 5(1):101-116.**

**4. **Ameghino, Florentino** (1883) - Sobre una nueva colección de mamíferos fósiles recogidos por el profesor Scalabrini en las barrancas del Paraná.
*Boletín de la Academia Nacional de Ciencias*, Córdoba. 5:257-306.**

**5. **Ameghino, Florentino** (1883) - Geología argentina.
*La Patria Argentina*, March 14, 1883.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-02-24 **Last updated:** 2018-08-03
1997 Vertebrate Paleontology Reference List

**1987 1988 1989 1990 1991 1992 1993 1994 1995 1996 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007**

* A-L
* M-Z

* A-0
* B-0
* C-0
* D-0
* E-0
* F-0
* G-0
* H-0
* I-0
* J-0
* K-0
* L-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-06-30 **Last updated:** 2018-06-30
Additions to the Fish Fauna of N.W. Europe. 3. Three new species of the genus Scyliorhinus from the Late Cretaceous (Campanian and Maastrichtian) of the Limburg area (Belgium and The Netherlands)

* Description
* Abstract
* Described species (0)
* New species (3)
* References (54)

**Teeth of *Scyliorhinus biddlei* sp. nov., *Scyliorhinus luypaertsi* sp. nov. from the Late Cretaceous (Late Maastrichtian, Maastricht Formation) and *Scyliorhinus reyndersi* sp. nov. from the Late Cretaceous (Late Campanian, Gulpen Formation) of Belgium and The Netherlands are described and illustrated. The new species, together with *Scyliorhinus antiquus* (AGASSIZ, 1843), *Scyliorhinus elongatus* (DAVIS, 1887), *Scyliorhinus fossilis* (LERICHE, 1927 non PROBST, 1879) and *Scyliorhinus coupatezi* HERMAN (1974), are separated from all other fossil species previously described as ?Scyliorhinus and reassigned to the genus Scyliorhinus sensu stricto.**

 **2** | ***Scyliorhinus reyndersi* sp. nov.** | 84-88
 **3** | ***Scyliorhinus luypaertsi* sp. nov.** | 89-

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2016-03-25 **Last updated:** 2018-06-05
1584 Vertebrate Paleontology Reference List

**1574 1575 1576 1577 1578 1579 1580 1581 1582 1583 1585 1586 1587 1588 1589 1590 1591 1592 1593 1594**

* O-1

**1. Olivus, Joannes Baptista (1584) - *De reconditis et praecipuis collectaneis ab honestissimo et solertissimo Francisco Calceolario Veronense in Musaco adservatis*.
Venice. 22 + 54 + 16 pp.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-06-03 **Last updated:** 2018-06-03
Bonefish-otoliths from the Anversian (Middle Miocene) of Antwerp

* Description
* Abstract
* Described species ( )
* New species ( )
* References (29)

**The faunas from the ‘Zanden van Antwerpen’ (Sands of Antwerp) and the ‘Zanden van Edegem’ (Sands ofEdegem), which make up the Anversian, are compared: the latter is older and the fauna preferred an environment close to the coast or shallow marine; the former, younger formation was formed in slightly deeper water further from the coast. The numerous otoliths of deep-sea fishes in the Sands of Antwerp must be allochthonous, although how these otoliths came to be there is still unknown.**
**One new species is described here, viz. *Trisopterus antwerpiensis*. This species is compared with the closely related *T. benedeni* biometrically.**
**The otoliths of the Sands of Antwerp confirm an age of uppermost Middle Miocene for this formation. Lowermost Middle Miocene for the Sands of Edegem is not contradicted by the otoliths found there.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-01-08 **Last updated:** 2018-07-05
2002 Vertebrate Paleontology Reference List

**1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012**

* A-L
* M-Z

* A-0
* B-0
* C-0
* D-0
* E-0
* F-0
* G-0
* H-0
* I-0
* J-0
* K-0
* L-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

* M-0
* N-0
* O-0
* P-0
* Q-0
* R-0
* S-0
* T-0
* U-0
* V-0
* W-0
* X-0
* Y-0
* Z-0

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**1.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2018-05-20 **Last updated:** 2018-08-02
An early Eocene fish fauna from the Bitter Creek area of the Wasatch Formation of southwestern Wyoming, U.S.A.

**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 (89)

**Early Eocene fluvial ichthyofaunas of Wyoming are relatively poorly known compared with the better-preserved lake deposits of the Green River Formation. We describe the teleost fishes from a single floodplain locality in the main body of the Wasatch Formation that immediately predates the formation of Lake Gosiute, in the Washakie Basin of Wyoming. This assemblage was deposited during the Graybullian substage of the Wasatchian Stage, corresponding to the onset of the rapid climatic warming leading to the Early Eocene Climatic Optimum. In addition to a lepisosteiform and an amiid, the locality has a teleost ichthyofauna comprising *Diplomystus* (Ellimmichthyiformes), a gonorynchiform probably representing Notogoneus, amblyopsid-like percopsiforms that may represent up to three taxa, and perciforms among which are probably an indeterminate centrarchid and ‘Priscacara.’ The fauna demonstrates that many of the Green River Formation fish taxa were already present in fluvial environments prior to the formation of the Green River lakes, indicating that the subsequent climate warming had little effect on these fishes. Some of the elements recognized here as probably representing Notogoneus were previously recovered from Late Cretaceous deposits from Utah to Alberta, suggesting that this gonorynchid was wide-ranging in North American fluvial environments since Mesozoic times, as were several other taxa identified here. Furthermore, the ichthyofauna indicates that the depositional environment was well vegetated and well oxygenated. These waters were shallow, with gentle flow strengths, which, together with the high oxygen content, suggests that the sediments of the locality were deposited in small ponds connected to an active river system.**

**Copyright © JPP-Journals Wikia, 2014-2022**
**Created :** 2017-11-06 **Last updated:** 2018-06-09