Notice bibliographique
Résumé
Mycale (Mycale) loveni (Fristedt, 1887) (Figs. 2 and 3 and Table 1) SYNONYMS: Clathria loveni Fristedt, 1887, Esperella bellabellensis Lambe, 1905, Esperella fisheri de Laubenfels, 1926, Esperia loveni (Fristedt, 1887), Myclae (Carmia) bellabellensis (Lambe, 1905), Mycale bellabellensis (Lambe, 1905), Mycale fisheri (de Laubenfels, 1926), and Mycale loveni (Fristedt, 1887). DIAGNOSIS: Stalked sponge with a cavernous funnel- or tubeshaped body, though specimens may be highly polymorphic and attain massive forms. Sponge body varies in size from a few centimetres in length to over one metre in funnel-shaped specimens. Generally found in deep water (> 200 m), though the holotype (22 m) and other specimens have been collected in shallow water (Fristedt 1887). The sponge body varies in size from a few centimetres in length to over one metre in funnel-shaped specimens. MATERIALS EXAMINED: Mycale cf. bellabellensis (Lambe, 1905), RBCM 978-00084 - 002, Edge of Clayoquot Canyon, British Columbia, Canada, 48.955 ◦ N, 126.415 ◦ W, 201 m depth, collected by PBS/JAT, 26 May 1962. Mycale (Mycale) loveni (Fristedt, 1887), RBCM 003-00036 - 002, off southern Alaska, USA, 55.883 ◦ N, 153.75 ◦ W, 228 m depth, collected by PBS, 1963. Mycale (Mycale) loveni (Fristedt, 1887), RBCM 009-00134 - 005, Dixon Entrance, British Columbia, Canada, 54.45 ◦ N, 131.7 ◦ W, collected by Pacific Biological Station (PBS), 12 August 1965. Mycale (Mycale) loveni (Fristedt, 1887), NA086-086-03, West of Olympic Peninsula, Washington, USA, 48.2503 ◦ N, 125.0129 ◦ W, 257 m depth, collected by NOAA, 26 August 2017. Mycale (Mycale) loveni (Fristedt, 1887), NA086-102, West of Olympic Peninsula, Washington, USA, 48.129 ◦ N, 125.084 ◦ W, 276 m depth, collected by NOAA, 28 August 2017. Mycale (Mycale) loveni (Fristedt, 1887), NA086-103-01, West of Olympic Peninsula, Washington, USA, 48.129 ◦ N, 125.084 ◦ W, 276 m depth, collected by NOAA, 28 August 2017. Mycale (Mycale) loveni (Fristedt, 1887), SH1812-039, Daisy Bank, off Salem Oregon USA, 44.665 ◦ N, 124.809 ◦ W, 342 m depth, collected by NOAA, 15 October 2018. Mycale (Mycale) loveni (Fristedt, 1887), SH1812-091, Mendocino Ridge, northern California, USA, 40.2873 ◦ N, 124.6901 ◦ W, 364 m depth, collected by NOAA, 20 October 2018. Mycale (Mycale) loveni (Fristedt, 1887), SH1812-190, Santa Lucia Bank, central California, USA, 34.679 ◦ N, 121.172 ◦ W, 549 m depth, collected by NOAA, 1 November 2018. Mycale (Mycale) loveni (Fristedt, 1887), SH1812-245, Sverdrup Bank, southern California, USA, 33.140 ◦ N, 120.356 ◦ W, 263 m depth, collected by NOAA, 6 November 2018. Mycale (Mycale) loveni (Fristedt, 1887), RL1905-069B, Wind Farm West, central California, USA, 35.062 ◦ N, 121.532 ◦ W, 706 m depth, collected by NOAA, 30 October 2019. Mycale (Mycale) loveni (Fristedt, 1887), NA121-057B, Quinault Canyon, WA, USA, 47.2179 ◦ N, 124.9047 ◦ W, 325 m depth, collected by NOAA, 27 September 2020. Mycale (Mycale) loveni (Fristedt, 1887), NA121-145B, Grays Canyon, Washington, USA, 46.9137 ◦ N, 124.8914 ◦ W, 294 m depth, collected by NOAA, 1 October 2020. COMPARATIVE MATERIAL EXAMINED: Syntype: Esperella bellabellensis Lambe, 1905, CMNI 1994-0038 / CMNI 1994-0039, off Bella Bella, Campbell Island, British Columbia, Canada, 52.17 ◦ N, 128.17 ◦ W, 549 m, collected by F. Landsberg, 1904. EXTERNAL APPEARANCE (Figs. 2A, 2B, 2D, 3A, 3B, and 3C): The external morphology of Mycale (Mycale) loveni is variable. Most authors report M. (M.) loveni as being stalked, though some Gulf of Alaska specimens were reported as massive (Stone et al. 2011). Fristedt’s (1887) original description from the Chukchi Sea depicts branching, thickly stalked specimens where lateral branches form subquadrangular cells filled with softer macerated tissue. Koltun (1959) reported Russian specimens (Chukchi, Bering, and Okhotsk Seas) with broad funnel-shaped stalks, though some specimens lack the large funnel. The surface is rough and may be grooved or microhispid. The colour while alive is greenish yellow to light yellow to brown. Consistency is somewhat compressible; it is not easily torn across spicule tracts, but smaller spicule tracts can be teased apart. Sponge tissue is easily removed from between the thick skeletal fibres and may be absent upon collection. Table 1 lists the outer morphologies that were examined and those from literature sources. SKELETON (Fig. 2C): The choanosome is composed of branching and anastomosing thick, multispicular tracts composed of styles echinated at varying intervals by loose styles. Between these thick tracts, secondary tracts form polygonal reticulations 1200–1600 µm across, often partly infilled with style brushes. Anisochelae are concentrated on the surface of spicule tracts and scattered throughout. Spicule tracts expand into plumes at the surface, and spicules protrude 100– 200 µm beyond the surface singly or in groups. At the surface, tangential tracts of styles cross-connect these plumes, forming a polygonal reticulation with meshes highly variable in shape and dimension, from 300 to 1200 µm in diameter. Large anisochelae form rosettes that occur sparingly in the ectosome and choanosome. Single large and small anisochelae are scattered throughout the sponge and are concentrated in the outer tissue layer that covers living specimens.Funnel Bering Strait, Eastern Aleutians – 350–465 72–100 35 – Note: n = 30 measurements of individual spicules unless otherwise noted. ∗ From literature sources. SPICULES (Figs. 2E–2L and 3D–3K and Table 1): From examined specimens, the spicule complement consists of styles as megascleres and anisochelae microscleres, usually clearly divisible into three size classes, each with somewhat different morphologies. Measurements from CMNI 1994-0038: Styles: 425– 456 –496 × 11– 13 –15.5 µm. Straight, sharp points may be lanceolate or mucronate. Styles either lack the constriction in the shaft just below the head found in most Mycale species (mycalostyles) or the constriction is slight. Large anisochelae: 83– 88 –94 µm. Frontal alae are narrow, and slightly rounded. The free portion of the shaft is approximately 1/4 of the total spicule length. Rosettes are variably present and scattered throughout the sponge. Medium anisochelae: 43– 54 –67 µm. Slight variations in shape are noted between a likely fan-shaped fragment (RBCM 003-00036-002, Figs. 2I and 2J) and a club-shaped specimen (RBCM 978-00084-002; Figs. 3H and 3I), where the alae are stouter in the club-shaped specimen. However, this variation is only visible at high magnification and may not be consistent between the two morphotypes. Small anisochelae: 19– 22 –25 µm. Elongated. In some spicules, there is a miniscule median tooth-like extension arising from the lower alae along the upper rim, but most often this upper rim is flat. GENETIC DATA: D13–E13 domains of 28S and ITS gene fragments were obtained from Pacific Mycale (Mycale) loveni specimens. Only about 40 bp overlapped in M. (M.) loveni ITS sequences due to low sequence quality from stutter artifacts following three successive homopolymer repeats greater than 9 bp in length (Fazekas et al. 2010). Maximum likelihood trees comparing available Mycale ITS and D13–E 13 28S sequences resulted in a monophyletic clade for M. (M.) loveni (Figs. 4 and 5). COI sequences for M. (M.) loveni were only obtained in one direction, so consensus sequences were not created; however, most of the top nucleotide BLAST search results for the single direction reads were members of the genus Mycale. DISTRIBUTION AND ECOLOGY: Mycale (Mycale) loveni has a very wide distribution range that spans the Arctic and North Pacific oceans. The holotype originates from the Chukchi Sea (Fig. 1A), with records also identified from the Bering Sea, Aleutian Islands, Gulf of Alaska, and British Columbia, between 22 and 800 m depth. Records from NOAA’s national database for deep-sea corals and sponges (Hourigan et al. 2015) show M. (M.) loveni to be particularly common around the Aleutian Islands and the Gulf of Alaska, which reflects the historical sampling intensity in this region. There are also sparse records as far south as California, within the Monterey Bay National Marine Sanctuary (Hourigan et al. 2015). From ROV observations off British Columbia, Canada, in situ sponges were commonly attached to hard substratum ranging in size from small cobbles to exposed bedrock. The usual stalked morphology of M. (M.) loveni may allow this species to inhabit areas inimical to sponge growth once the larvae successfully settle. Mycale (Mycale) loveni was observed to be a common, large, habitat-forming demosponge at Learmonth Bank, Dixon Entrance in sites that were dominated by the abundance of several large glass sponge species, notably Farrea sp., Aphrocallistes vastus (Schulze, 1886) and Heterochone calyx (Schulze, 1886) (Chu 2010). Other fauna co-occurring with M. (M.) loveni include Sebastes spp. rockfish, alcyonacean corals such as Primnoa pacifica Kinoshita, 1907, cup corals, other small corals, crinoids, anemones, holothurians, brachiopods, and sponges (Chu 2010). REMARKS: The specimens analyzed here are consistent with Fristedt’s (1887) original description of C. loveni. Fristedt described an erect and irregularly ramous specimen with several slender branches issuing from a firm stalk, and the branches form a mesh that is filled with softer tissue. The styles of this species were described to be thickest near the pointed end, and this holds true for most of the examined specimens; however, the more hastate spicules as described by Koltun (1959) are not present in all specimens. Here we also suggest that the species has three size categories of anisochelae rather than two. This is contrary to Fristedt’s original description, which does not mention a small size category, while de Laubenfels (1932) reported four size categories for large specimens that he considered as Mycale bellabellensis. In most specimens, the separation of
Récupéré en direct depuis OpenAlex et désinversé. Les résumés ne sont pas conservés dans cette base de données : les index inversés représentent 8,6 Go des 9,3 Go de texte de la base, et le serveur dispose de 13 Go libres.
Comment cette classification a été obtenuedéplier
Prédiction machine sur la base complète
Imitation des enseignantsNi prévalence calibrée, ni vérité terrain. Validation humaine à venir. Le volet Gemma est une étiquette directe du modèle pour chaque travail de la base, lue sur la notice réduite au titre. Le volet Codex est un classifieur appris des 10 348 étiquettes directes de Codex et calibré sur les taux pondérés de l'échantillon; les champs sans appui suffisant ne portent aucun appel Codex. Le mode candidate est l'union des deux volets; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont pas des étiquettes humaines.
Scores du classifieur distillé par catégorie (deux têtes)
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,000 | 0,000 |
| Méta-épidémiologie (sens strict) | 0,000 | 0,000 |
| Méta-épidémiologie (sens large) | 0,000 | 0,000 |
| Bibliométrie | 0,001 | 0,000 |
| Études des sciences et des technologies | 0,001 | 0,000 |
| Communication savante | 0,000 | 0,001 |
| Science ouverte | 0,000 | 0,001 |
| Intégrité de la recherche | 0,000 | 0,000 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,008 | 0,002 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découleClassification
machine, non validéePrédiction automatique; un appel candidat d’une seule source (Gemma direct ou Codex distillé), pas un consensus.
Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».