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A New Hemichordate, Saccoglossus bromophenolosus (Hemichordata, Enteropneusta, Harrimaniidae), From North america PDF

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PROC. BIOL. SOC. WASH. 107(2), 1994, pp. 383-390 A NEW HEMICHORDATE, SACCOGLOSSUS BROMOPHENOLOSUS (HEMICHORDATA: ENTEROPNEUSTA: HARRIMANIIDAE), FROM NORTH AMERICA Gary M. King, Cem Giray, and Irv Komfield Abstract.—Anew species, S. bromophenolosus, isdistinguishedfrom its con- gener, S. kowalevskii (Agassiz 1873), on the basis ofthe following morpholog- ical, biochemical, and genetic criteria: placement ofgill pores; prominence of the dorsal ridge; structure ofthe proboscis skeleton; presence ofbromophenols or bromopyrroles; relative electrophoretic mobility ofallozymes (e.g., super- oxidedismutase);molecularweightsoffragmentsfromrestrictionendonuclease digestion of mitochondrial DNA. S. bromophenolosus occurs from southern Maine,U.S.A.,toNovaScotia, Canada,withanadditionalrecordfromWillapa Bay, Washington, U.S.A. Three families of enteropneusts (Hemi- tionsaboutthe taxonomic status ofthe spe- chordata: Enteropneusta: Harrimaniidae, cies (King 1986, Woodin et al. 1987). Spe- Ptychoderidae, and Spengeliidae) occur cifically, animals collected in Maine and along the coasts of North America (Milne northward typically accumulate high con- & Milne 1973, Bullock 197.S, Ruppert & centrations oftwo secondary products, 2,4- Fox 1988). The best known species belong dibromophenol andadibromoindole (King to the genus Saccoglossus (Harrimaniidae), 1986, unpubl. data), while animals from which occurs on both the Atlantic and Pa- other locales accumulate 2,3,4-tribromo- cific coasts (Milne & Milne 1973, Bullock pyrrole (King, unpubl. data, Woodin et al. 1975). Ofthe several saccoglossids, S. ko- 1987). Thedifferentialaccumulationofthese walevskii(Agassiz 1873) has beendescribed haloaromatics does not appear to correlate in greatest detail. Various aspects ofits dis- with any major environmental variables or tribution, biology and ecology have been gradients. Further, the presence ofa given reportedsubsequentto Agassiz's(1873)ini- haloaromatic phenotype appears to be a tial description (e.g., Bateson 1886, Bullock fixedtraitassociated with populations from 1940, Tweedell 1961, Colwin & Colwin specific regions. 1962, Barrington 1965, King 1986, Woodin We now report that the genus Saccoglos- et al. 1987, Balser & Ruppert 1990, Carey sus consists ofat least two distinct species & Mayer 1990). S. kowalevskii has been along the Atlantic coast ofNorth America. considered the only memberofitsgenus on These two species are readily differentiated the Atlantic coast of North America, and by gross external morphological characters, hasbeennotedinintertidalcollectionsfrom the accumulation of halogenated aromatic Nova Scotia to Georgia (Dorjes 1972, compounds, morphology of the proboscis Bromley 1979). Although there are certain skeleton, electrophoretic mobilities ofsev- characteristics common to all saccoglossids eral enzymes, and the sequence composi- along this range, a comparison ofbiochem- tion ofthe mitochondrial DNAs (mtDNA). icalattributesreportedforpopulationsfrom We propose the name S. bromophenolosus Maine and South Carolina has raised ques- forthe newspeciesoccurringfrom southern 384 PROCEEDINGS OFTHE BIOLOGICALSOCIETY OFWASHINGTON Mainenorthwardandpossessingfeaturesas boscides was irritated with the syringe nee- detailed below. S. kowalevskii occurs from dle prior to sample collection in order to southern Maine southward, as noted by stimulatemucusandhaloorganicexcretion. Verrill (1873) and Gosner (1979). The samples were analyzed by direct injec- tion into a gas chromatograph. Details of the extraction and analytical procedures Materials and Methods have been reported elsewhere (King 1986, Saccoglossids were collected from the in- 1988). The proboscideal skeletons of 5 in- tertidal zones ofsites ranging from Halifax, dividuals from Lowes Cove and York, Nova Scotia, to Georgetown, South Caro- Maine, were examined after dissection of lina, by excavating sediments to a depth of live animals. about 10 cm at low tide. The proboscis, collarandanteriorportionsofthetrunkwere Saccoglossus bromophenolosus, obtained readily by removing the animals new species directly from the substrate, but complete Figs. 1-4, Table 1 specimensweredifficulttocollectduetothe Saccoglossussp. Bullock 1975, p. 619; Koz- fragilityofthe posteriorregion ofthetrunk. loff 1987, p. 478. Specimens were examined in the field for Saccoglossus kowalevskii.—Milne & Milne external morphological characteristics (see 1973, (p.p.): 230; Bromley 1979, p. 533. below)andthenplacedindividuallyin small Saccoglossus kowalewskyi.—Brinkhurst et vials (20 ml) containing local seawater; the al., 1976, p. 156. animals were subsequently transported to Saccoglossus kowalevskyi.—¥Ang, 1986, p. Walpole, Maine, for further processing. 257. MtDNA was extracted from live animals — Saccoglossuskowalewskii. Linkletteretal. using procedures modified from Lansman 1977, (p.p.): 42, Gosner 1979, p. 265; letabaol.ra(t1o9r8y1.)Awimthiinni2m4u-m48ofh1o0frleivteuranntiomatlhse Meinkoth, 1981, (p.p.): 726; Carey & Mayer, 1990, p. 79. from Lowes Cove and York, Maine (69°34'N, 43°56'W; 43°09'N, 70°39'W) and Diagnosis.—Saccoglossus bromopheno- from Portsmouth, New Hampshire losusattains a length up to 20 cm. It has an (43°06'N, 70°42'W) were also homogenized elongate proboscis thatextends 1.5-2 cm in for electrophoretic analyses of enzymes at narcotized specimens. The proboscis has a the following loci using standard methods shallow dorsal groove and a single pore at (Murphy et al. 1990): glucose phosphate the base of the proboscis. Concretions fill isomerase (GPI; E.C. 5.3.1.9), malate de- the primary shaft ofthe proboscis skeleton. hydrogenase (MDH; E.C. 1.1.1.37), phos- Hexaneextractsoftheprobosciscontain2,4- phoglucomutase (PGM; E.C. 2.7.5.1), and dibromophenol andadibromoindole; these superoxidedismutase(SOD; E.C. 1.15.1.1). compounds account for the characteristic Analyses of haloorganic contents utilized "bromoform" odor oflive specimens. The extracts ofanimalsthat were extractedwith collar is diiferentiated into 4-5 zones, and hexane immediately aftercollection and re- is generally rectangular from above with an moval of adhering sediment. In addition, aspectratioofabout 3:5 (width length). The : animals used for mtDNA and allozyme trunk is differentiated into distinct bran- analyses were "halotyped" by collecting 1- chial and hepatic-genital regions. Dorsolat- 2-jLtl samples of the seawater immediately erally placed gill pores appear ellipsoid in adjacent to the proboscis with a 10-jul gas relaxed and ventilating specimens, with the chromatography syringe (Hamilton Inc., majoraxis oriented vertically: the gill pores Reno, Nevada). The epidermis ofthe pro- do not occur in folds and vary from about VOLUME 107, NUMBER 2 385 60-110 pair per individual. Esophageal dorsolaterally, beginning at thejunction of pores, which occur slightly posterior to the collar and trunk. Slightly posterior to the gill pores vary from about 4-8 pairin num- terminal gill pores, 4 pairs ofdorsal esoph- ber. Gonads begin at the terminus of the ageal pores were observed; they formed an branchial region in both sexes, and are dor- angleofabout30°openingtowardthetrunk. solateral in placement. The hepatic-genital region ofthe trunk ex- Material examined.—YioXoiypt (USNM tended about 23 mm, measured from the 168049) and 3 paratypes (USNM 168050- terminationofthegillporestoapointwhere 168052)fromLowesCove, Maine(69°34'N, genital structures were not observable. Na- 43°56'W), collected by G.M. King 20 Oc- scent grayish egg masses were visible dor- tober, 1993. solaterallyjust beneath the epidermis. The Description.—The holotype is a sexually hepatic-genital region was grayish-brown immature female with the following char- dorsallyandyellowish-brownlaterally. The acteristics observed while the animal was posterior-most region of the trunk was 34 mm relaxed in a solution of7% MgCl2. The in- inlength, yellowish-brown incolorand mm complete specimen was 82 in length; characterized by pairs of carmine-colored mm an additional 60-70 of the posterior- spots located dorsally. most region ofthe trunk was lost unavoid- General dimensions for 3 male paratypes ably during collection. The posterior-most with maturing gonads were similarto those section ofthe trunk was extremelythin and oftheholotype. However,gillporenumbers fragile; in color and diameter, it resembled ranged between 68-101 and esophageal the fecal coils present at the sediment sur- pores numbered 4-6. The sperm sacs were face. The relaxed and extended proboscis dorsolateral and pink in color. was creamy white in color with a shallow Remarks.—AXihou^ the range of body dorsal groove running from the base to the size, coloration, location and appearance of proboscistip. Striationsperpendiculartothe the gonads, and external features ofthe col- major axis ofthe proboscis were observed larandproboscisof-S. bromophenolosusand at low power on a dissecting microscope. S. kowalevskii are very similar, gill pore mm The proboscis was 16 in length and 3 placementandthemorphologyofthedorsal mm at the base. The basal-most region was ridge allowdiscrimination ofthe species by arustorangeincolor. Theorangecollarwas visual inspection in the laboratory or field mm mm 5 in length and 2.5 and 3 in di- (Fig. 1, 2). In contrast to S. bromopheno- ameter at the anterior and posterior ends, losus, the dorsal ridge of S. kowalevskii is respectively. Both ends of the collar were relatively broad and flattened immediately distinctlythickened,withaprominentlight- posterior to the collar, covering >50% of er-colored ridge circlingthe posteriorofthe the dorsal area. The dorsolateral gill pores collar.Thebranchialregionofthetrunkwas ofS. kowalevskiioccurwithinlateralgrooves mm about 2.5 in diameter where it joined that can be closed, thereby obscuring them the posterior of the collar. A prominent, from view (Fig. 2). This state is typical of raised dorsal ridge began immediately pos- specimens preserved without prior relaxa- terior to the collar and ran the length ofthe tion. Inadditionto external morphology, S. branchial region, terminating just anterior bromophenolosusand S. kowalevskiican be totheesophagealpores. Nearthe collar, the distinguished by other diagnostic charac- mm dorsal ridge was about 1 in width with teristics requiring dissection orvarious lab- mm a central groove about 0.5 in width. oratory analyses (Fig. 3, Table 1). Collec- Thisregion ofthetrunkwaspinkish-orange tionstodateindicatethatS. kowalevskiiand to orange and about 14 mm in length. A S. bromophenolosusexistsympatrically only total of 61 pairs ofgill pores were located within a narrow range around the mouth of 386 PROCEEDINGSOFTHE BIOLOGICALSOCIETY OFWASHINGTON Fig. I. A. Dorsolateral view of relaxed, sexually immature female of 5. hroniophenolosus. new species illustratingsuperficialfeaturesoftheproboscis(P),collar(C,limitsindicatedbyarrows)andtrunk(T);gillpores (gp, indicated by arrow) are evident immediately posterior to the collar. B. Detailed view ofthe posterior proboscis, collar, and anteriorofthetrunk, illustratingtheprominent, raised dorsal ridge (DR)and gill pores. VOLUME NUMBER 107, 2 Fig. 2. Anterior portion ofS. kowalevskii showing the broad, flattened dorsal ridge (DR), collar (C) and proboscis (P); gill poresare obscuredby lateral folds (F, indicatedbyarrow). The "sole" (S) occurs ventrally. the Piscataqua River, New Hampshire S. kowalevskii since GPI, MDH, and PGM (43°06'N, 70°42'W); S. kowalevskii has not were fixed for alternative, diagnostic alleles been observed north ofYork, Maine, while within each taxon; SOD was represented at 5". bromophenolosus has not been found 2 monomorphic loci in S. bromophenolo- south ofPortsmouth, New Hampshire. sus, andbyasingle, differentmonomorphic AUozyme analyses indicated substantial locus in S. kowalevskii. MtDNA analyses divergencebetweenS. bromophenolosusand alsorevealedsubstantialdivergence(Fig. 4). Table 1.—Diagnosticcharactersthatdistinguishamong 3 speciesofNorth Atlantic saccoglossids. S.bromophenolosus S.kowalevskii S.ruber Characteristic Dorsal ridge raised, narrow broad, flattened raised, narrow Gill pore placement central lateral central Coloration' (proboscis-collar-trunk) W/P-O/R-O W/P-O/R-O P/R/R-O Halotype^ DBP/DBI TBPy DBP/TBP Proboscis skeleton^ narrowcurve-co broadcurve-no co narrowcurve-co ' Colorcode:W/R,rangesfromwhitetopalepink;O/R, rangesfromorangetored;O,orange;P/R,palepink to pale red. ^Compoundcode:DBP=2,4-dibromophenol;DBI=dibromoindole(positionsofbromineatomsuncertain); TBP = 2,4,6-tribromophenol; TBPy = 2,3,4-tribromopyrrole. ' Co refersto concretionswithinthe proboscis skeleton. 1 388 PROCEEDINGS OFTHE BIOLOGICALSOCIETY OFWASHINGTON B Fig. 4. Autoradiogram offragments from the di- gestionofpooledmtDNAfromspecimensof5.bromo- phenolosus, new species (lanes 1, 3) or 5. kowalevskii (lanes2,4)withtherestrictionendonucleasesHindIII (lanes 1, 2) or Sty I (lanes 3, 4). Fragments were sep- aratedafterdigestionbyagarosegelelectrophoresisand radiolabelled with "S using a nick translation proce- dure. Lane 5 containsa molecularweight standard ( kbladder, BRL); "a"and "b"indicate 5090and 1018 base pair fragments, respectively. Fig. 3. A. Diagram oftheproboscideal skeleton of 5'. bwmophcnolosiis. new species; dark central region consists ofconcretions as described forS. ruber(Bur- don-Jones& Patil 1960). B. Diagram oftheproboscis skeletonofS. kowalevskii;noteabsenceofcentralcon- cretionsand more deeply curved skeletal arms. VOLUME 107, NUMBER 2 389 No common DNAfragments werefoundin Grant for assistance with collections from comparisonsofrestriction endonucleasedi- Nova Scotia; Drs. E. Ruppert and D. Hub- gests ofthe mtDNA ofthe two taxa based bard for information about and assistance on Hind III, Xba I, Nde I, Sty I, Stu I, Dra with collections from Georgetown, South I or Ava I. In contrast, mtDNA haplotypes Carolina;A. LaursenandDrs. C. Planteand for populations ofeach taxon were homog- G. Kozloff for information about and col- enous. Forexample, an Xba I digestyielded lections of specimens from Willapa Bay, the followingapproximate fragment molec- Washington. This work was partially sup- ular weights: S. bromophenolosus—Sl50, ported by funds from the National Science 1075, 925, and 625, 5. kowalevskii-5000, Foundation, OCE-9203342 and EHR91- 3225, 2275, 1875, and 1000. 08766. Etymology.—The species name is de- rived from its characteristic haloorganic Literature Cited content, 2,4-dibromophenol, and the Latin suffix,-05M5; thus S. bromophenolosus, Sac- Agassiz, A. 1873. The history ofbalanoglossus and tomaria.—MemoirsoftheAmerican Academy coglossus "with bromophenol." Distribution.—Onthe eastcoast ofNorth Balser,oEf.ArJ.t,s&ScEi.enEc.eRIuXp:p4e2r1t.^291.990. Structure, ul- America, the range ofS. bromophenolosus trastructure, and function ofthe preoral heart- extends north from the mouth of the Pis- kidneyin Saccoglossuskowalevskii(Hemichor- cataqua River separating Maine and New data, Enteropneusta)includingnewdataon the HampshiretoatleastHalifax, NovaScotia. Harringsttono,moEc.hoJ.rdW..—Ac1t9a65Z.oolToghiecabi7o1l:o2g3y5-o2f49h.emi- S. bromophenolosus is found in silty sands chordataandprotochordata.W.J.FreemanCo., throughoutthe intertidalzone inthisrange. San Francisco. 176 pp. It is often distributed in patches, with den- Bateson, W. 1886. Continued account ofthe later sitiesfrom about 10-> 100 individualsm"^. stagesinthedevelopmentofBalanoglossusko- In addition, a sub-tidal form has been re- walevskii, and ofthe morphology ofthe Enter- opneusta.-Quarterly Journal of Microscopical corded from the Damariscotta River Science 26:511-533. (69°34'N, 43°56'W) at a depth of 10-20 m. Brinkhurst, R. O., L. E. Linkletter, E. I. Lord, G. A. Specimens obtained from Willapa Bay, Conners, & M. J. Dadswell. 1976. A prelim- Washington(46°37'N, 124°00'W)havevery inary guide to the littoral and subtidal marine similarDmNtADNA haplotypes and 16S ribo- imnavnertMeabrrianteesLaobforPaatsosray.maStq.uAondddryewBsa,y.N.HBu.nt1s66- somal sequences (pers. observations); pp. in addition, the external morphologies and Bromley, J. E. C. 1979. A preliminary checklist of haloorganiccontents ofthese organismsare marinefauna ofMinas BasicandMinasChan- indistinguishable from S. bromophenolosus nel—Proceedings ofthe Nova Scotia Institute ofScience 29:517-541. (K. Woodwick, in litt.). Since these north- Bullock, T. H. 1940. Thefunctionalorganization of western Pacific saccoglossids represent a the nervous system ofEnteropneusta.-Biolog- previouslyunnamedspecies(Kozloff1987), ical Bulletin 79:91-113. we incorporate them as trans-Arctic repre- . 1975. Phylum Hemichordata. Pp. 618-619 sentatives of5". bromophenolosus. The range in R. L Smith & J. T. Carlton, eds.. Light's ofthewesternNorthAmerican populations manual: intertidal invertebrates ofthe Central CaliforniaCoast, 3rded. UniversityofCalifor- is uncertain, but appears to include Oregon nia Press, Berkeley, 716 pp. and Washington (Bullock 1975, Kozloff Burdon-Jones,C. 1951. Observationsonthespawn- 1987). ing behaviour ofSaccoglossus horsti Brambell — and Goodhart, and ofother Enteropneusta. Acknowledgments JournaloftheMarineBiologicalAssociationof GMK the United Kingdom 29:625-638. memory doefdiHc.atWe.s tKhiinsg.maWneusctrhiapntk tDor.thJe. S,a&ccAo.glMo.ssPuastil(.En1t9e6r0o.pneAusrteav)isiionnoBrfitthieshgewnau-s 390 PROCEEDINGS OFTHE BIOLOGICALSOCIETY OFWASHINGTON ters.—Proceedings ofthe Zoological Society of Meinkoth, N. A. 1981. The Audubon Society field London 134:635-645. guide to North American seashore creatures. Carey, D. A.,&L. M. Mayer. 1990. Nutrientuptake A.A. Knopf, NewYork, 813 pp. by a deposit-feedingenteropneust: nitrogenous Milne, L. & M. Milne. 1973. InvertebratesofNorth sources.—Marine Ecology Progress Series 63: America. Doubleday, Inc., NewYork, 249 pp. 79-84. Murphy, R. W., J. W. Sites, Jr., D. G. Buth, & C. H. Colwin, L. H., & A. H. Colwin. 1962. Induction of Hanfler. 1990. Proteins I: isozyme electro- spawning in Saccoglossus kowalevskii (Enter- phoresis. Pp. 45-126 in D. M. Hillis&C. Mo- opneusta) at Woods Hole.—Biological Bulletin ritz, eds.. Molecular Systematics. Sinauer As- 123:493. sociates, Inc., Sunderland, Massachusetts, 588 Dorjes, J. 1972. Georgia coastal region, Sapelo Is- pp. land, U.S.A.: sedimentology and biology. VII. Ruppert, E. E., &R. S. Fox. 1988. Seashoreanimals distribution and zonation ofmacrobenthic an- ofthe southeast. University ofSouth Carolina imals.—Senckenbergiana maritima 4:169-182. Press, Columbia, 429 pp. Gosner, K. L. 1979. A field guide to the Atlantic Tweedell, K. S. 1961. Regeneration ofthe enterop- seashore.HoughtonMifflinCo.,Boston,329pp. neust, Saccoglossus kowalevskii.—Biological King, G. M. 1986. Inhibition ofmicrobial activity Bulletin 120:118-127. in marine sedimentsby abromophenol from a Woodin, S. A., M. D. Walla, & D. E. Lincoln. 1987. hemichordate.—Nature 323:257-259. Occurrence ofbrominated compounds in soft- . 1988. Dehalogenation in marine sediments bottom benthic organisms.—Journal ofExper- containing natural sources of halophenols.— imental Marine Biology and Ecology 107:209- Applied and Environmental Microbiology 54: 217. 3079-3085. Verrill,A. E. 1873. ExplorationsofCascoBaybythe Kozloff, E. N. 1987. MarineinvertebratesofthePa- U.S. Fish.Comm.B.NaturalHistory.Proceed- cificNorthwest.UniversityofWashingtonPress, ings ofthe American Association for the Ad- Seattle, Washington, 511 pp. vancement ofScience pp. 340-395. Lansman, R. A., R. O. Shade, J. F. Shapiro, & J. C. cAlveiassee.s t1o981m.easTuhreeusmeitoofchroensdtrriicatlionDeNnAdonsue-- (GMK and CG) Darling Marine Center quence relatedness in natural populations. III. and Center for Marine Studies, University Techniques and potential applications.—Jour- of Maine, Walpole, Maine 04573, U.S.A.; nal ofMolecularEvolution 17:214-226. (IK) Department ofZoology and Centerfor LinklettAerc,heLc.klEi.,stEo.fI.maLroirnd,e&fauMn.aJa.nDdafdlsowrealolf.the19B7a7y. Marine Studies, University of Maine, of Fundy. Huntsman Marine Laboratory. St. Orono, Maine 04469, U.S.A. Contribution Stevens, New Brunswick, 68 pp. 268 from the Darling Marine Center.

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