Stylet jaws of Chrysopetalidae (Annelida) Author Watson, Charlotte Author Faulwetter, Sarah text Journal of Natural History 2017 2017-11-24 51 47 - 48 2863 2924 http://dx.doi.org/10.1080/00222933.2017.1395919 journal article 10.1080/00222933.2017.1395919 1464-5262 5184119 Genus Paleaequor Watson Russell, 1986 ( Figure 11a–d , 12a, b ; Tables 1 , 2 ) Type species: Paleaequor setula Watson Russell, 1986 Material examined Two specimens Paleaequor nicoyensis Watson Russell, 1986 NTM . W. 25482, Peru , Eastern Pacific (mCT-00152, mCT-00170); 4 specimens Paleaequor setula NTM W . 2053, Queensland , Australia , South West Pacific (mCT-00017, mCT-00090, mCT-00095, mCT- 00107); Paleaequor breve ( Gallardo, 1968 ) NTM W . 25392, Malaysia , Eastern China Sea . Distribution Paleaequor species are found in tropical to sub-tropical waters in world oceans between 37°N and 30°S . Figure 10. Hyalopale cf. bispinosa (mCT-00039), imaged through micro-CT and rendered in 3D. (a) dorsal view, entire body; (b and c) dorsal view, virtually dissected at different levels to expose pharyngeal structures; (d) jaws, dorsal view and cross sections through the jaw along its length; Hyalopale bispinosa microscope figures: (e) anterior end of animal, dorsal view; (f) jaws, dorsal view. Figure 11. Anterior end of Paleaequor setula (mCT-00090), imaged through micro-CT and rendered in 3D. (a) dorsal view; (b, c and d) dorsal view, virtually dissected at different levels to expose pharyngeal structures. (c and d) false-colour volume rendering, colours represent different densities. Warm colours: higher densities, cold colours: lower densities. Habitat The taxon is frequently found in tropical estuaries, sand flats and submarine banks at the entrances to rivers; intertidal to> 80 m . Paleaequor species have been almost exclusively recorded from sediments ranging from shell and gravel to fine sand and muds with a high organic content as well as from silty reefs ( Watson Russell 1986 ). Large numbers of Paleaequor nicoyensis were recorded from the eastern side of the Gulf of Nicoya from stations located off river mouths with high freshwater and detrital run-off during the wet season ( Maurer and Vargas 1984 ). Within soft substrates Paleaequor species are associated with biogenic reef habitats made up of tube-dwelling polychaetes. Wilson (1979) describes Paleaequor heteroseta ( Hartman, 1945 ) as one of the most dominant species found in maldanid sedimentary reefs. Polgar et al. (2015) categorize Paleaequor breve as an opportunistic species present in the pre-settlement phase of sabellariid reef building when the sedimentary surface is characterized by mud deposits being reworked by the dominant surface deposit feeder, the terebellid Loimia verrucosa Caullery, 1944 . Figure 12. Paleaequor breve , dissected pharynx and jaws. (a) microscope picture; (b) line drawing. General morphology Paleaequor species are relatively slender chrysopetalids with the dorsum completely covered by flattened, golden-brown coloured, notochaetal paleal fans; main paleae possess raised ribs and tubercules ( Figure 11a ). Paleaequor species attain short to moderate lengths, e.g. Paleaequor heteroseta , 7 mm length for 63 segments; Paleaequor breve , 18 mm length for 118 segments. Sensory structures include a small retractile prostomium (fused with anterior segments) in association with a nuchal fold, two pairs of complex eyes, cylindrical palps, lateral organs and retractile styles of dorsal cirri. Ventral pads are present ( Watson Russell 1986 , figures 2–7; CW pers. obs.). Pharynx and jaws Paleaequor possesses a proboscis that when retracted appears to be divided, with possibly two associated lobes ( Figure 11d ), and when closer to eversion appears more slender ( Figure 12a, b ). A long, slender partly differentiated pharynx extends to approximately segment 20 and posterior caeca are present. CT scans illustrate a short rounded anterior pharynx wherein the stylets sit (stylets not visible in CT scans), followed posteriorly by a tight constriction that takes the form of a characteristic ‘kink’ ( Figure 11d ; Watson Russell 1986 ). The pharyngeal juncture formed by this constriction is overlain with extensive, twisted glands: both major (mj. gl.) and minor (mn. gl.) in diameter and length. In dorsal view, the major glands extend longitudinally both anteriorly and posteriorly from the juncture along the pharynx ( Figure 11b, c ); segmental minor glands extend horizontally into the parapodia along the length of the pharynx ( Figure 11c, d ). Jaws are fragile in composition with no identifiable calcification and are only visible under a compound microscope; small stylets are very slender with attenuated distal tips (lacking serration), straight margins, slightly flaring basal ends and moderately wide inner grooves ( Figure 12a, b ).