{"title":"Rethinking holotypes: how environmental silicon shapes sponge skeletons and their taxonomic interpretation","authors":"","doi":"10.1093/zoolinnean/zlag157","DOIUrl":"https://doi.org/10.1093/zoolinnean/zlag157","url":null,"abstract":"<span class=\"paragraphSection\">Routine taxonomic identification of sponges (phylum Porifera) relies largely on skeletal features and, despite the development of molecular markers, the skeletal approach persists because of its practicality. However, skeletal variability of uncertain origin often complicates species-level diagnoses. Using three common Mediterranean siliceous sponges, we experimentally demonstrate that environmental concentrations of silicic acid (dSi)—the raw material used by sponges for skeleton formation—is a major driver of skeletal diversity, significantly influencing the diversity of skeletal elements (spicules) produced and their dimensions. Most wild individuals of these three demosponges exhibit underdeveloped spicule inventories in their natural habitats, which are characterized by low dSi concentrations (∼1 µM). When transferred to laboratory conditions with experimentally elevated environmental dSi (up to 100 µM), sponges develop more complex spicule inventories. The experimentally induced skeletal differences are so pronounced that low-dSi and high-dSi conspecifics could easily be misidentified as different species in skeletal-based studies. The findings further suggest that shallow-water siliceous demosponges, systematically outcompeted by diatoms in terms of dSi uptake, frequently encounter dSi concentrations in their habitats below the threshold required for full skeleton development. Importantly, this effect extends to museum-stored holotypes. Holotypes originating from sites with unusually high dSi relative to the mean across the species’ distribution range are likely to produce fully developed skeletons that do not match the naturally underdeveloped skeletons prevailing in most conspecifics. Conversely, holotypes from habitats with average dSi concentrations across the species’ natural distribution range (typically low dSi) will more accurately represent the skeleton found in most individuals, although this skeleton will probably correspond to an underdeveloped version of the species’ full skeletal potential. Sponge biologists need to rethink the way in which sponge species are represented by their holotypes and how holotype skeletal traits can be better used for species’ diagnosis. Holotype studies should be systematically contextualized through assessment of dSi concentrations at the type locality and across the species’ distribution ranges.</span>","PeriodicalId":49333,"journal":{"name":"Zoological Journal of the Linnean Society","volume":"30 1","pages":""},"PeriodicalIF":2.8,"publicationDate":"2026-10-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"149221503","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"生物学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Alfred A J Lemierre,James D Gardner,Márton Venczel,Vlad Codrea,Jason S Anderson,Zoltán Szentesi
{"title":"A frog with horns in the Late Cretaceous: new information on\u0000 Hungarobatrachus szukacsi\u0000 (Neobatrachia: Anura)","authors":"Alfred A J Lemierre,James D Gardner,Márton Venczel,Vlad Codrea,Jason S Anderson,Zoltán Szentesi","doi":"10.1093/zoolinnean/zlag154","DOIUrl":"https://doi.org/10.1093/zoolinnean/zlag154","url":null,"abstract":"Abstract The Late Cretaceous Hungarobatrachus szukacsi from Hungary is the only Mesozoic neobatrachian species known in Laurasia. Previously represented by isolated and incomplete ilia (including the holotype), tibio-fibulae, maxillae, squamosals, angulosplenials, and frontoparietals, Hungarobatrachus szukacsi has been regarded as a possible ranoid or hyloid. A recently discovered, three-dimensional skull of Hungarobatrachus szukacsi preserves the paired otoccipitals and squamosals, an incomplete left pterygoid, and posterior portions of the parasphenoid and fused frontoparietals in articulation. The new skull shows an unexpected and rare feature: the dorsal, posterolateral corners bear a horn-like paraoccipital process formed by a posterior elongation of the processus posterdorsalis and processus dorsalis of the squamosal. Elsewhere among anurans, paraoccipital processes occur in just two other neobatrachian genera (all species of Hemiphracus and several species of Ceratophrys), but the composition and form of paraoccipital processes differ among the three taxa. Our new cladistic analyses suggest that Hungarobatrachus szukacsi and four other Late Cretaceous neobatrachian species, two each from South America and Africa, may be australobatrachians, yet are not members of either the less inclusive Calyptocephalellidae or Myobatrachoidea. If correct, this result indicates that australobatrachians were more diverse and widely distributed during the Late Cretaceous than previously recognized.","PeriodicalId":49333,"journal":{"name":"Zoological Journal of the Linnean Society","volume":"28 1","pages":""},"PeriodicalIF":2.8,"publicationDate":"2026-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"149150778","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"生物学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}