Pegmatothylakos manumii, McLoughlin, Bomfleur, Mörs & Reguero, 2016

McLoughlin, Stephen, Bomfleur, Benjamin, Mörs, Thomas & Reguero, Marcelo, 2016, Fossil clitellate annelid cocoons and their microbiological inclusions from the Eocene of Seymour Island, Antarctica, Palaeontologia Electronica 11 (1), pp. 1-27 : 13

publication ID

https://doi.org/ 10.26879/607

publication LSID

lsid:zoobank.org:pub:42B578E7-5E4C-42FF-A24C-B5671CBD903E

persistent identifier

https://treatment.plazi.org/id/21970058-1A59-424A-855E-CE1BAEE14E9A

taxon LSID

lsid:zoobank.org:act:21970058-1A59-424A-855E-CE1BAEE14E9A

treatment provided by

Felipe

scientific name

Pegmatothylakos manumii
status

sp. nov.

Pegmatothylakos manumii sp. nov.

Figures 4.7-9; 8 View FIGURE 4 View FIGURE 5 View FIGURE 6 View FIGURE 7 View FIGURE 8 View FIGURE 9

zoobank.org/ 21970058-1A59-424A-855E-CE1BAEE14E9A

Holotype. NRMS089730 ( Figures 4.7-9; 8 View FIGURE 4 View FIGURE 5 View FIGURE 6 View FIGURE 7 View FIGURE 8 View FIGURE 9 ).

Type Locality, Stratum, and Age. Locality: IAA 1/ 90; ‘ Natica horizon’ within the Cucullaea I Allomember (Telm 5) of the La Meseta Formation; early Eocene.

Additional Material. NRMS 089734, locality: IAA 2/95; ‘ Natica horizon’ within the Cucullaea I Allomember (Telm 5) of the La Meseta Formation; early Eocene.

Etymology. After Professor Svein Bendik Manum (1926–2015), Norwegian palaeobotanist, who carried out the first major survey of fossil clitellate annelid cocoons.

Diagnosis. Cocoon ellipsoidal, <6 mm long. Pegmatine dark brown to black in reflected light, consisting of a semi-regular reticulum of girders enclosing circular, elliptical, or rounded-polygonal lumina mostly ~ 75–200 μm in diameter. Girders consisting of a core of fibrous or hackly material coated on the lateral and interior surfaces by multiple flattened strips of smooth, tightly overlapping threads. Hapsine amber-coloured, consisting of loosely interwoven slender threads.

Description. Cocoon ellipsoidal ( Figure 4.7 View FIGURE 4 , 8.1 View FIGURE 8 ); 4.6 mm in preserved length (estimated complete length ~ 5 mm), ~ 3 mm in equatorial diameter, circular in cross-section except where crushed; anterior end broadly rounded; posterior end damaged in all examples but potentially operculate ( Figure 4.8 View FIGURE 4 ). Outer shell (pegmatine) consisting of a semi-regular reticulate network of girders enclosing roughly equidimensional (rounded-polygonal, broadly elliptical, or circular) lumina with maximum dimensions of 50–220 μm ( Figures 4.9 View FIGURE 4 , 8.2 View FIGURE 8 ). Girders consisting of two components—a core of brown fibrous or hackly material 20–35 μm thick ( Figure 8.6 View FIGURE 8 ), and a lateral- and interior-surface coating of multiple flattened strips of subsequently secreted dark brown to black glossy dense threads that tightly overlap ( Figure 8.3-5 View FIGURE 8 ) and locally bifurcate in complex arrangements ( Figure 8.7 View FIGURE 8 ). Girders are ~ 50 μm thick and 50–80 μm wide. Rare spermatozoal fragments and other inclusions are entrapped between the laminar threads coating the inner surface of the pegmatine girders (described below).

Hapsine positioned to the interior side of the pegmatine but not obviously attached. Hapsine weakly developed, consisting of slender (2–8 μm diameter), amber-coloured, cylindrical, sparsely branched threads arranged in a loose, complex interwoven felt-like meshwork ( Figure 8.8 View FIGURE 8 ).

Remarks. Only two specimens are available of this newly described taxon, but its unique architecture incorporating a robust pegmatine reticulum enables the species to be readily differentiated from all other fossil clitellate annelid cocoons. Attribution to Clitellata is based on the presence of a hapsine layer, apparently operculate character, and the sporadic occurrence of diagnostic spermatozoa inclusions embedded between the pegmatine filaments.

The pupal sacs of some Diptera, Coleoptera , Lepidoptera , and Neuroptera are enveloped by an external meshwork that is somewhat reminiscent of the pegmatine layer of Pegmatothylakos . However, such pupal casings are constructed in an essentially woven manner, i.e., having a succession of continuous threads that are superimposed in moreor-less opposite directions and subsequently connected. By contrast, the pegmatine in Pegmatothylakos has multiple layers of threads delineating individual rounded-polygonal lumina without any apparent hierarchical relationship in girder structure. We hypothesize that the formation of the pegmatine may—unlike that of a woven or otherwise coordinated construction—result, at least in part, from the self-organization of the girders on some ephemeral scaffold, possibly a mucous foam- or bubble-layer, at the time of cocoon secretion. Additional differences are the more variable and greater size of the lumina in the reticulum of insect pupal casings, and the much greater separation of the reticulum from the inner pupal sac (see, e.g., Eiseman and Charney, 2010; Holland, 2010).

Some insect eggs (especially those of lepidopterans) also have morphologies superficially similar to the reticulate structure of Pegmatothylakos ( Sourakov and Emmel, 1995; Dunn, 2010), and several examples of ornate Mesozoic insect eggs have recently been described in detail (e.g., Pott et al., 2008; Heřmanová and Kvaček, 2010; Heřmanová et al., 2013; Fisher and Watson, 2015). However, both modern and fossil insect eggs have complex wall anatomies and surface morphologies with reiterating patterns ( Hinton, 1970, 1981; Ren, 1992; Wolf and Reid, 2001; Fisher and Watson, 2015) that allow their differentiation from annelid cocoons.

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