scholarly journals A type catalogue of the reed frogs (Amphibia, Anura, Hyperoliidae) in the collection of the Museum für Naturkunde Berlin (ZMB) with comments on historical collectors and expeditions

2021 ◽  
Vol 97 (2) ◽  
pp. 407-450
Author(s):  
Frank Tillack ◽  
Ronald de Ruiter ◽  
Mark-Oliver Rödel
Keyword(s):  
Historical Research ◽  
Type Specimens ◽  
The Family

We present a commented catalogue of the type specimens of the Afro-Malagasy frog family Hyperoliidae at the herpetological collection of the Museum für Naturkunde Berlin (ZMB). In current publications and databases, many names based on ZMB primary types are listed as synonyms of other species, the types often declared as lost. Consequently, the respective names are often no longer considered in current taxonomic work. We traced 146 nominal taxa of the family Hyperoliidae in the ZMB collection of which currently 130 are presented by primary types (88 holotypes, 10 lectotypes and 32 taxa based on syntype series); 50 of these taxa are currently considered as valid. Primary types of nine taxa could not be located during our inventory of the collection holdings. Seven taxa are exclusively represented by secondary types (paratypes). Many of these types comprise taxa where types have been thought to be lost. As a further service to the community, we provide important details about collectors and their travel routes, as well as respective documents stored in the collection of the Department of Historical Research at ZMB. This should make it easier to potentially compare the ZMB types in future taxonomic revisions.

Early Paleozoic Hyolitha from North America: reexamination of Walcott's and Resser's type specimens

1988 ◽  
Vol 62 (2) ◽  
pp. 218-233 ◽  
Author(s):  
John Mark Malinky
Keyword(s):  
North America ◽  
Lower Cambrian ◽  
Type Species ◽  
New Genus ◽  
Early Paleozoic ◽  
Type Specimens ◽  
Middle Cambrian ◽  
Upper Cambrian ◽  
New Family ◽  
The Family

Concepts of the family Hyolithidae Nicholson fide Fisher and the genera Hyolithes Eichwald and Orthotheca Novak have been expanded through time to encompass a variety of morphologically dissimilar shells. The Hyolithidae is here considered to include only those hyolithid species which have a rounded (convex) dorsum; slopes on the dorsum are inflated, and the venter may be flat or slightly inflated. Hyolithes encompasses species which possess a low dorsum and a prominent longitudinal sulcus along each edge of the dorsum; the ligula is short and the apertural rim is flared. The emended concept of Orthotheca includes only those species of orthothecid hyoliths which have a subtriangular transverse outline and longitudinal lirae covering the shell on both dorsum and venter.Eighteen species of Hyolithes and one species of Orthotheca from the Appalachian region and Western Interior were reexamined in light of more modern taxonomic concepts and standards of quality for type material. Reexamination of type specimens of H. similis Walcott from the Lower Cambrian of Newfoundland, H. whitei Resser from the Lower Cambrian of Nevada, H. billingsi Walcott from the Lower Cambrian of Nevada, H. gallatinensis Resser from the Upper Cambrian of Wyoming, and H. partitus Resser from the Middle Cambrian of Alabama indicates that none of these species represents Hyolithes. Hyolithes similis is here included under the new genus Similotheca, in the new family Similothecidae. Hyolithes whitei is designated as the type species of the new genus Nevadotheca, to which H. billingsi may also belong. Hyolithes gallatinensis is referred to Burithes Missarzhevsky with question, and H. partitus may represent Joachimilites Marek. The type or types of H. attenuatus Walcott, H. cecrops Walcott, H. comptus Howell, H. cowanensis Resser, H. curticei Resser, H. idahoensis Resser, H. prolixus Resser, H. resseri Howell, H. shaleri Walcott, H. terranovicus Walcott, and H. wanneri Resser and Howell lack shells and/or other taxonomically important features such as a complete aperture, rendering the diagnoses of these species incomplete. Their names should only be used for the type specimens until better preserved topotypes become available for study. Morphology of the types of H.? corrugatus Walcott and “Orthotheca” sola Resser does not support placement in the Hyolitha; the affinities of these species are uncertain.

scholarly journals New species of the genus Otitoma Jousseaume, 1898 (Pseudomelatomidae, Conoidea) from the Western Pacific Ocean

2017 ◽  
Author(s):  
Mauro Morassi ◽  
Andrea Nappo ◽  
Antonio Bonfitto
Keyword(s):  
New Species ◽  
Pacific Ocean ◽  
New Caledonia ◽  
The Philippines ◽  
Western Pacific Ocean ◽  
Type Specimens ◽  
Fiji Islands ◽  
The Family ◽  
First Time ◽  
The Western Pacific

Twelve new species are assigned to the genus Otitoma Jousseaume, 1898 in the family Pseudomelatomidae Morrison, 1966 and herein described: O. hadra sp. nov., O. neocaledonica sp. nov., O. rubiginostoma sp. nov and O. tropispira sp. nov. from New Caledonia; O. boucheti sp. nov., O. nereidum sp. nov. and O. sororcula sp. nov. from the Fiji Islands; O. xantholineata sp. nov. from the Solomon to the Fiji Islands; O. crassivaricosa sp. nov. from Fiji to Hiva Oa Island (Marquesas Archipelago); O. philpoppei sp. nov. from the Philippines but also reported from the Fiji Islands; O. elegans sp. nov. from the Fiji Islands and O. philippinensis sp. nov. from the Philippines. New data on O. carnicolor (Hervier, 1896) are provided. Otitoma mitra (Kilburn, 1986), from Southern Mozambique, is here considered a synonym of O. cyclophora (Deshayes, 1863). Drillia batjanensis Schepman, 1913, previously assigned to the genus Maoritomella Powell, 1942 in the family Borsoniidae Bellardi, 1875, is here assigned to the genus Otitoma. Photographs of the holotype of Drillia batjanensis are provided for the first time. In addition, color photographs of the type specimens of the following species are provided: Drillia kwandangensis Schepman, 1913, D. timorensis Schepman, 1913 and Mitrellatoma mitra Kilburn, 1986.

Phylogenetic relationships of the Balkan Moitessieriidae (Caenogastropoda: Truncatelloidea)

Zootaxa ◽  
2018 ◽  
Vol 4486 (3) ◽  
pp. 311 ◽  
Author(s):  
SEBASTIAN HOFMAN ◽  
ALEKSANDRA RYSIEWSKA ◽  
ARTUR OSIKOWSKI ◽  
JOZEF GREGO ◽  
BORIS SKET ◽  
...  
Keyword(s):  
Dna Sequences ◽  
Phylogenetic Relationships ◽  
Shell Morphology ◽  
Type Specimens ◽  
Diagnostic Features ◽  
The Balkans ◽  
The Family ◽  
Species Type ◽  
A Site ◽  
Subterranean Waters

The family Moitessieriidae includes minute dioecious gastropods exclusively inhabiting subterranean waters, including thermal ones. Only empty shells were collected in most species, the vast majority of them are described from their gross shell morphology alone. Several visits to a site are usually required to obtain at least some living individuals. High variability in shell morphology and the lack of diagnostic features, coupled with anticipated high levels of endemism, has resulted in a long list of nominal moitessierid species. Type specimens stored as empty shells omit unambiguous identification and delimitation of species boundaries. Due to inaccessibility of cave animals and consequent lack of material suitable for molecular analysis, the phylogenetic relationships, as well as the taxonomy of the family at genus/species level, are far from being understood. The anatomy of the family is also poorly known and provided only for a few taxa. The distinctness of the Moitessieriidae has sometimes been questioned, and their monophyly not proved. Twelve species of the Balkan Moitessieriidae are considered: two species of Paladilhiopsis, two species of Bythiospeum, six species of Iglica, Costellina turrita and Lanzaia bosnica. The shell morphology of each species, as well as the reproductive system of Paladilhiopsis and Iglica, were analysed. DNA sequences of nuclear histone H3, ribosomal 18S, ribosomal 28S and mitochondrial cytochrome oxidase subunit I (COI) were applied to infer phylogenetic relationships among the taxa. The sequences of Bythiospeum from GenBank have been used to infer relationships between Bythiospeum and Paladilhiopsis that were recently synonymized. Paladilhiopsis and Iglica are distinct, but closely related genera, as is the genus Bythiospeum, which does not occur in the Balkans. Its relationships with both former taxa remain unresolved. The Moitessieriidae are clearly distinct from all other families of the Truncatelloidea, however, their monophyly remains doubtful. 

Lectotypification of Sematophyllum latifolium, a new synonym of Wijkia surcularis (Pylaisiadelphaceae, Bryophyta)

Phytotaxa ◽  
2021 ◽  
Vol 484 (3) ◽  
pp. 298-300
Author(s):  
NARIN PRINTARAKUL ◽  
SAHUT CHANTANAORRAPINT
Keyword(s):  
Type Specimen ◽  
Common Species ◽  
Type Material ◽  
Type Collection ◽  
Type Specimens ◽  
Northern Thailand ◽  
New Synonym ◽  
The Family

Sematophyllum latifolium Brotherus (1911: 362), known only from the type collection, was originally described by Brotherus (1911) based on a collection made by C.C. Hosseus from Mt. Doi Suthep (Doi Sutäp), in northern Thailand. Pollawatn (2008) revised the family Sematophyllaceae s.l. in Thailand but did not see the type specimen of S. latifolium. During the study of Hosseus’s collections, however, we found two duplicates of type specimens of S. latifolium one located in H-BR and one in M. We found that several critical features of S. latifolium, such as the 1) irregular-pinnately branching habit with the erect flagelliform branches (Fig. 1A), 2) stem and branch leaves strongly differentiated (Fig. 1B−F), and 3) brotherelloid type alar cells often divided into larger hyaline cells towards leaf margins (Fig. 1G), were indistinguishable from those in the type material of Wijkia surcularis (Mitten 1859: 112) Crum (1971: 173), a common species found growing from India to Indochina (Gangulee 1980; Tan & Iwatsuki 1993; Tan & Jia 1999; Jia et al. 2005). Thus, we here propose S. latifolium as a new synonym of W. sucularis. In the protologue, Brotherus (1911) did not designate the holotype, therefore, it is necessary to select a lectotype for S. latifolium ((see Art. 9.11 of the Shenzhen Code (Turland et al. 2017)). We designate Hosseus’s collection (Hosseus s.n.) in H-BR (H) as the lectotype of the name S. latifolium.

Does Gender Matter?

2008 ◽  
pp. 54-71
Author(s):  
Paula E. Hyman
Keyword(s):  
Critical Analysis ◽  
Jewish History ◽  
Women's History ◽  
Historical Research ◽  
The Holocaust ◽  
The Family ◽  
European Jewish ◽  
Gender Based ◽  
And Gender ◽  
Women’S History

This chapter probes the significant contributions to the understanding of the past, which postmodern criticism that has attributed vital importance to women as a historical subject and to gender as a category of critical analysis. It offers a valuable assessment both of inroads already made by women's history and gender analysis into Jewish historical research. It also invokes distinctions drawn by Gerda Lerner, 'the doyenne of women's history', to categorize both achievements and desiderata in the field of feminism. The chapter reviews compensatory history which focuses on women previously ignored, including gender-based adjustment and refinement of interpretation in areas ranging from the Conversos to the shtetl and from the Holocaust to the family. It tackles areas where women's and gender-sensitive history have the power to transform and reshape the fundamental assumptions of European Jewish history.

Mesodiphthera Tillyard, 1919, from the Late Triassic of Queensland, the oldest cicada (Hemiptera: Cicadomorpha: Cicadoidea: Tettigarctidae)

Zootaxa ◽  
2019 ◽  
Vol 4567 (2) ◽  
pp. 358 ◽  
Author(s):  
KEVIN J. LAMBKIN
Keyword(s):  
Basal Cell ◽  
Structural Diversity ◽  
Wide Distribution ◽  
Nodal Line ◽  
Late Triassic ◽  
Type Specimens ◽  
Fossil Insect ◽  
The Family ◽  
New Material ◽  
Cross Vein

New specimens of its type species from the Queensland Late Triassic (Norian) (~227–~208.5 Ma) fossil insect locality at Dinmore have revealed that the old and obscure Late Triassic genus Mesodiphthera Tillyard, 1919, from nearby Denmark Hill, is a tettigarctid cicada, the earliest record of the family and the oldest cicada. The genus is distinguished by the combined presence of three characters: the primary forks of R and M at about the same level, midway between the basal cell and the nodal line; RA2 with four or five terminal branches; and the inter-medial cross-vein backwardly inclined, running between M2 and M3. Of the three species originally ascribed to Mesodiphthera by Tillyard, only its type, M. grandis Tillyard, 1919, is retained in the genus. The other two species differ significantly from the type and are transferred to Tardilly gen. nov., which is similar to Mesodiphthera in the more or less aligned primary forks of R and M placed at about midway between the basal cell and the nodal line, and the backwardly inclined inter-medial cross-vein which runs between M2 and M3. It differs, however, in its smaller size, broader costal space, three-branched M3+4, and differently shaped CuA and CuA2. The new material, all of which is of M. grandis, provides a complete picture of the shape, colour and venation of its tegmen, whereas Tardilly prosboloides (Tillyard) comb. nov., 1922 and Tardilly dunstani (Tillyard) comb. nov., 1922 are still known only from their poorly preserved type specimens. Mesodiphthera and Tardilly exhibit a number of presumed plesiomorphies, viz the costal space much wider than the CuA cell, the basal cell strongly narrowed apically, and the post-nodal cross-vein series closer to the nodal line than the apex, which place it in the probable paraphyletic subfamily Cicadoprosbolinae. A more informed assessment of their relationships, however, must await a comprehensive analysis of the now 29 fossil genera of the family. The Tettigarctidae were the only cicadas of the Mesozoic and the discovery in the Triassic of Australia of Mesodiphthera and Tardilly clearly distinct from the 24 previously known Mesozoic genera, further demonstrates the family’s high degree of structural diversity, and emphasises its almost world-wide distribution in that Era. 

William Bulloch, 1868 - 1941

1941 ◽  
Vol 3 (10) ◽  
pp. 819-852
Keyword(s):  
Historical Research ◽  
Literary Critic ◽  
Emeritus Professor ◽  
Main Interest ◽  
The Past ◽  
London Hospital ◽  
The Family ◽  
History Of ◽  
The University ◽  
The City

William Bulloch, Emeritus Professor of Bacteriology in the University of London and Consulting Bacteriologist to the London Hospital since his retirement in 1934, died on n February 1941, in his old hospital, following a small operation for which he had been admitted three days before. By his death a quite unique personality is lost to medicine, and to bacteriology an exponent whose work throughout the past fifty years in many fields, but particularly in the history of his subject, has gained for him wide repute. Bulloch was born on 19 August 1868 in Aberdeen, being the younger son of John Bulloch (1837-1913) and his wife Mary Malcolm (1835-1899) in a family of two sons and two daughters. His brother, John Malcolm Bulloch, M.A., LL.D. (1867-1938), was a well-known journalist and literary critic in London, whose love for his adopted city and its hurry and scurry was equalled only by his passionate devotion to the city of his birth and its ancient university. On the family gravestone he is described as Critic, Poet, Historian, and indeed he was all three, for the main interest of his life outside his profession of literary critic was antiquarian, genealogical and historical research, while in his earlier days he was a facile and clever fashioner of verse and one of the founders of the ever popular Scottish Students’ Song Book .

A new genus of ichthyosaur from the Late Triassic Pardonet Formation of British Columbia: bridging the Triassic Jurassic gap

2001 ◽  
Vol 38 (6) ◽  
pp. 983-1002 ◽  
Author(s):  
Elizabeth L Nicholls ◽  
Makoto Manabe
Keyword(s):  
British Columbia ◽  
Type Species ◽  
New Genus ◽  
Late Triassic ◽  
Unique Combination ◽  
Type Specimens ◽  
Nomen Dubium ◽  
The Family ◽  
Large Diamond

Both the genus Shastasaurus and the family Shastasauridae have long been hard to define due to the fragmentary nature of the type specimens. Consequently, recent interpretations of the genus have been based almost entirely on Shastasaurus neoscapularis from the Late Triassic Pardonet Formation of British Columbia. Two new specimens of this taxon, from Pink Mountain, British Columbia, demonstrate that it does not belong in the genus Shastasaurus. This paper describes the new specimens, and refers the species to Metashastasaurus gen nov. Post-cranially, the skeleton of Metashastasaurus resembles that of shastasaurids, differing primarily only in the shape of the scapula and fibula. However, the skull has a unique combination of characters, including large diamond-shaped frontals that enter the supratemporal fenestrae, and very narrow posterior extensions of the nasals, which contact the postfrontals. It also differs from the skull of Shastasaurus in the presence of both a parietal ridge and postparietal shelf. This is a combination of derived characters previously known only in Jurassic forms. The front limb has four proximal carpals and four digits, indicating that previous reconstructions were based on incomplete material. Shastasaurus pacificus Merriam 1895, the type species of the genus Shastasaurus, must be considered a nomen dubium, making the genus Shastasaurus invalid. Until this problem is clarified, the use of the generic name Shastasaurus should be restricted to Merriam's type specimens, of which only Shastasaurus alexandrae and Shastasaurus osmonti are based on adequate material.

Taphonomic bias and the evolutionary history of the family Cidaridae (Echinodermata: Echinoidea)

Paleobiology ◽  
1992 ◽  
Vol 18 (1) ◽  
pp. 50-79 ◽  
Author(s):  
Benjamin J. Greenstein
Keyword(s):  
Type Species ◽  
Evolutionary History ◽  
Middle Triassic ◽  
Upper Jurassic ◽  
Late Triassic ◽  
Type Specimens ◽  
Fossil Material ◽  
Group I ◽  
The Family ◽  
History Of

The class Echinoidea apparently originated during the Ordovician Period and diversified slowly through the Paleozoic Era. The clade then mushroomed in diversity beginning in Late Triassic time and continued expanding into the present. Although this evolutionary history is generally accepted, the taphonomic overprint affecting it has not been explored. To gain a more accurate perception of the evolutionary history of the group, I have compared the diversity history of the family Cidaridae (Echinodermata: Echinoidea) with the preservational style of fossil type species using literature-derived data. The Cidaridae apparently originated in Middle Triassic time and diversified slowly through the Neocomian (Early Cretaceous). Diversity was maintained through the remainder of the Cretaceous and Tertiary Periods, reflecting the diversity history of the subclass. Characterization of the preservational style of type fossil material for the family revealed the following breakdown of preservational states: 60% of species were described on the basis of disarticulated skeletal material, primarily spines; 20% based on intact coronas denuded of spines, apical system, Aristotle's lantern and peristomial plates; 10% based on large coronal fragments; and 10% based on other skeletal elements. This distribution may represent the effect of a disarticulation threshold on the condition of echinoid carcasses before final burial and suggests that preservation of intact specimens may be very unlikely. For cidaroids, previous work has suggested that this threshold is likely to be reached after 7 days of decay.Comparison of the diversity history of the Cidaridae with the preservation data reveals that characteristic patterns of taphonomic overprint have affected the group since its origination in Middle Triassic time, and the nature of that overprint has changed over time: the early diversity history of the group is characterized by occurrences of fragmented fossil material, with spines predominant; further radiation of the group in mid-Jurassic time coincided with an increase in modes of preservation, ranging between exceptionally well-preserved material and disarticulated skeletal elements. Finally, type material is more rarely described from younger stratigraphic intervals (Miocene–Pleistocene) and consists predominantly of disarticulated skeletal elements and coronal fragments larger than an interambulacrum in size. Intact, denuded coronas are noticeably lacking.The number of type species of Cidaridae described in each stratigraphic interval has not been consistent during post-Paleozoic time. Middle Triassic, Malm (Upper Jurassic), Senonian (Upper Cretaceous) and Eocene series yielded significantly (α = .05) higher numbers of type specimens per million years, while the Lias (Lower Jurassic), Dogger (Mid-Jurassic), Lower Cretaceous and Paleocene yielded significantly (α = .05) lower numbers of type specimens per million years. This may be the result of a combination of taxonomic, sampling, and geographical biases.

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