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Praestorrsella roestae (Visser), a foraminiferal index fossil for Late Cretaceous deeper neritic deposits PDF

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Preview Praestorrsella roestae (Visser), a foraminiferal index fossil for Late Cretaceous deeper neritic deposits

213 Zitteliana Praestorrsellaroestaewasdiscoveredin1951byVissf.rinthe evidenceclearlybiasedbysuccessive,fundamentallydifferent typeMaestrichtian deposits and describedunderthe genenc interpretations. name Cibicides. Itwasclassified laterby Hofkerin 1955 as Thus, the purpose of this paper is to provide additional Lockhartiaandsubsequently(Hofker 1966)as Tremastegina documentationoftheexternalandinternalmorphologyofP. aGnodwtdhaus(t1r9a7n8s)ferrerterdanfsrfoemrrtehdetrhoetalsipiedcsietsottohetahmephriotsatleigiidns;idist.s ritosesstyaset'esmashteilcl,potsoitainoanl.yzeitsstructuralfeaturesandtodiscuss particulargenericnameexpressesitssupposedclosenesstothe Paleocene genus Storrsella. Loeblich & Tappan (1987) ThispaperisacontributiontoIGCPproject262.Fieldwork followed this opinion stressing however the need of more wassupportetintheframeworkofDGICYT-projectPB-90/ detailed and more objective morphological documentation. 0718. We thank Alfred Loeblich for providing a copy of The latter consists so far mainly of Hofker's drawings in Gowda'spaper(1978)publishedinIndia. several subsequent publications. They provide contradicting SYSTEMATIC DESCRIPTION 2. Praestorrsellaroestae(Visser,1951) Peripheryroundcdtoangular,ornamentedbytheperipheral PI. 1,Fig.1-19;PI.2,Fig.1-9;Text-Fig.1 endoftheventral imperforateridges. In theultimate halfor 1951 Cibicidesroestaen.sp.-Visser:291,pl.6,fig.9. bqeurasrtienrtwhheolralst,wthhoerpleroifpahdeurlytmspaeycibmecfnasinrtelayclhoibnuglaatbeo.ut120,C5hmamm- 1955 Lockhartiaroestae(Visser).-Hofker:4-5,fig.a-e. indiameter.Aperturenotobserved. 1959 Lockhartia roestae (Visser). - Hofker: 289-290, figs. 95-96. 1966 Tremasteginaroestae(Visser).-Hofker:24,figs.1-9. 2.2 ARCHITECTURE 1964b Rotalia(s.1.)roestae(Visser).-Gowda:308. (Text-Fig. 1) 1977 Tremasteginaroestae(Visser).-Villain:67. Thegrowthspiralofthisspeciesisverytightlycoiled:inthe 1978 Praestorrsella roestae(Visser). - Gowda: 3,fig.2 a-k, cquatorialzone,theradialextensionofthechamberlumenis fig.3a,b. notmuchmorethantwicethechamberheightinthedorsaland 1985 Tremasteginaroestae(Visser).-Drooger&deKlerk: less than twice the height of the ventral alar chamber ex- tensions. Dorsal part of the septum straight, inclined 1987 P1r2a0e,sptlo.rr1s,eflilga.1r.oestae(Visser). - Loeblich&Tappan: bexatceknwsairodnsofwitthherseespptecutmtvoerthyeldoiwr,ecrteiaocnhionfggtrhoewtahp.exDoirnsaalloaolsaer 662,pl.758,fig.7-11. coilofhalfavolution. Theshellhasanarrowumbilicalspacefilledwithagroupof 2.1 EXTERNALASPECTOFSHELL umbilicalpilesprotrudingmoreorlessfromtheventralsurface Comparativelysmall (about0,5 mm indiameter) lamellar- oftheshell. In the umbilical area, this surface is formed by perforate, trochospiral, involute, inequally biconvex, sub- fusedtriangulärfolia.Thefoliarnatureoftheumbilicalcover conicaltohemisphericaltest. can be recognized only in sections ofthe shell as the orna- mentationobscuresthesutures ofsubsequent folia. Residual Dorsal side hemispherical toconical, strongly ornatewith foliar apertures are kept open during growth ofsubsequent imperforate,thickpustulesarrangedinvaguelySpiralpattern; whorlsandproduceverticalcanalsopeningintotheambient dorsal chambersutures infewultimateChambers backwards environmentinbetweenumbilicalpiles. inclined,depressedorflush, inearlierChambersobscuredby ornamentation,visibleonlywhenthelateralchamberwallof Intercameral foramen consisting of a Single, low arch in thelastfewChambersiseroded.Thealarchamber-extensions inarginal-interiomarginalpositionatthebaseoftheseptalface. form loose spirals reaching the shell apex in about half a Thereisaseptalflapcoveringonlysmallpartsoftheseptal volution. Dorsal lateral chamber walls coarsely perforate faceintheventralpartoftheshell.Noseptalflapwasobserved inbetweenimperforate,heavypustulesreachingtheheightof onthedorsalpartoftheseptum.Theseptalflapmergesintoa thechamberlumeninthesubsequentshellwhorl. tinyumbilicalplateseparatingtheventralmainchamberlumen Ventralshellsurfaceconvexbutflattened,alwaysmuchless fromanumbilicalcavitySystem.Theumbilicalplateadmitsa convex than dorsal side. Septal sutures obscured by heavy single,large,roundedpassageconnectingtheventralchamber ornamentationcoveringtheventral,lateralchamberwallswith lumeninradialdirectionwiththeumbilicalcavities. radially directed, simple or outwardly forked, imperforate The strong ornamentation of the previous whorl by ridges alternating with narrow radial grooves carpeted with inflational pustules combined with the exceptionally low two or three rows of pore mouths. Towards the umbilical chambercavitiesproducepartialsubdivisionsofthechamber region,thegroovesfuseintoareticularpatternsimilartothe lumen. Ontheventralside,theradial ridgesontheprevious pattern of reticular zones in orbitolinids (but ofcourse not whorloecupyabouthalfoftheventralchamberlumeninthe homologouswithsuchastructure). next whorl. Their peripheral extensions however touch the 215 Fig. 1 A-D: Praestorrsella roestae (Visser). - Camera lucida drawings. Position ofsections seeA-D in legend, f: foramen, fol: folium, hs: hemiseptulum,s:septum,sf:septalflap,up:umbilicalplateproducinginsectionC„Shoulders"betweenwhichtheradialpassage(arrow)admits communicationbetweenmainchamberlumenandumbilicalcavities.AfromVilavellafm.,Pyrenees;Campanian.B-CfromSouthernIndia; Maastrichtian. very low ventral lateral walls and fuse with its inner lining 2.3DISTRIBUTION producing thus hemiseptula with a circular to oval cross- P. roestae is known so farfrom Maastricht (Netherlands, section.Thepreviouswhorl'spustulesonthedorsalsidetouch type localiryofthe Maestrichtian stage),the Pyrenean Basin thelowlateralwallsandsubdividethedorsalalarextensionsof and its margins south and north oftoday's mountain ränge, thechambercavitywithcylindricalhemiseptularelements.In from the Subbetic margin ofthe Betic Cordillieran Basin in contrast to the umbilical zone, the dorsal pusrules are Southern Spain (Sierra Seca, Granada; Azema et al. 1979: pl. intermittently superposed from one whorl to the next XL), and from Southern India (see in particular the list of producingonlvfcw,radialpilesoflamellae.Thedispositionof synonymies). In all those cases, P. roestae is associated to theumbilicalpustulesisstronglycoordinatedfromonewhorl orbitoidforaminiferaindicatingaMaestrichtianandpossibly to the next by superposition. The latter produces a regulär, also Campanian age. For more precision, a revision of the conical bündle of piles from the first to the last whorl. In- Campanian-Maestrichtianboundaryanditspositioninrespect berweenthepilesoflamellae,verticalumbilicalcanalsconnect oforbitoidevolutionwouldbenecessary. the cavities of superposed shell whorls. They are inter- connected by an horizontal network ofcanals derived from coveringthereticulargroovesontheventralshellsurfaceby 2.4OTHERSPECIES thenextwhorl. Gowda(1978)describedadditionaltwospeciesasbelonging Proloculus spherical, about 30 (im wide. No dimorphism tohisnewgenusPraestorrsella.ThematerialavailableinBasel observed. does not allow to recognize the two species. From the 216 somewhat summary description given by Gowda, it seems on theventral side, is not recognizable beyond this feature. veryprobablethatthesetwospeciesarenottobeplacedinthe Thus,forthetimebeing,Praestorrsellahastobeconsideredas genusPraestorrsella:P.reicheliGowdamaybeaDaviesinaor amonotypicgenus. asmallSiderolites,whileP.ariyalurensis,describedasevolute DISCUSSION 3. P. roestaehasaverysmallsize.Therefore,primarycements pondingto an areal, komma-shaped foramen(Hottingeret coating the cavities and/or outer shell surfaces hamper the al. 1991). Therefore, we interpret this element as umbilical analysis ofthe structural elements more than in larger-sized plate. isolated specimens and may obscure pores and passages. By Hofker's fig. 9 (1966) depicts stellar chamberlets on the combiningtheobservationsonrandomsectionsinhardrock, highlyconvexsideoftheshellasrevealedbychemicalerosion onorientedsectionsofisolatedspecimensandonSEMgraphs, oftheshellsurface. Forthisreason,heinterpretedthehighly wetrytodocumentthestructuralfeaturesofthisforminspite convexsideoftheshellasventralandaccordinglythecoilingas ofitssmallsize.However,thepreservationofthematerialdoes inverse-trochospiral. This is in Opposition to Hofker's own notpermitacloseanalysisofthelamellararchitecture. obliqueandequatorialsections(1966,fig.4,6)andtoourown Visser'sdescription from 1951 concernsonlytheourward observations.ThereisasimplespiralofuniserialChambersin aspect of shell morphology in this species. Hofker's Inter- this species. Therefore, P. roestae has no relations with pretation of its structure was based on sections of isolated amphistiginids. topotypes from Maastricht coated by primary cements NeithertheoriginalmanuscriptthesisofGowda(1964a)nor illustrated by camera lucida drawings. They agree with our itspartialpublication(Gowda 1978)produceinitsdrawings own observations as to chamber arrangement, as to the supplemcntary Information on P. roestae's structure. positionofthemarginal-intcriomarginalforamenandastothe AccordingtoGowda'sverbaldescription,Loeblich&Tap- existence of dorsal hemiseptula generated by pustules pan(1987)definethegenusPraestorrsellabyhaving„rotaliid supportingthelateralwallsofthenextwhorl'schamber.They intraseptalpassages"butnoexterna!suturalfissures.Whilethe alsoagreetosomeextentwiththeexistenceofatinycircum- latterfeatureisconfirmedbyallpreviousauthorsandourown umbilical cavity producing a kind of spiral canal by the observations, the existence of intraseptal passages without Separation of the main chamber lumen from the umbilical openings to the exterior is highly improbable: Intraseptal cavitySystembyanumbilicalplate. passages are partially closed, interlocular Spaces This latterelement was singled out in Hofker's drawings communicating always with the exterior. Our direct 4,7,8(1966)bystippledsurfacesinterpretedastooth-plates. observations on the shell do not confirm the existence of However, our material has not produeed intersections as intraseptal passages but the existence ofa septal flap tightly Hofker's fig. 8 (1966) comparable to Pararotalia and Neo- gluedtorestrictedpartsoftheseptalface. rotalia with a free edge of a true toothplate and corres- Plate1 Praestorrsellaroestae(Visser).-Lightmicroscope.Scalebar0,5mmvalidforallspecimens. Fig.1 Notquitecenteredaxialsectionoflargespeeimen.Alinyaformation,Montsec,SouthernPyrenees,Spain;LateCampanian(seealso CAUSetal.1988). Fig.2-3 Sectionsmoreorlessparalleltoandatvariousdistancesfromshellcoilingaxis.BeticCordillieras,Maastrichtian(seeAzEmaetal.1979, pl.40). Fig.4 Sectionperpendiculartocoilingaxis,throughdorsalpartofshell.Vilavellafm.,SantCorneliAnticline,Tremp,SouthernPyrenees; Campanian(seeGallemietal.1983). Fig.5 Sectionnotquiteperpendiculartocoilingaxis,centered.Noteproloculus.AlinyaEofSegreriver,SerradeTurp,seeCausetal.1988; LateCampanian. Fig. 6-7 Basalsections,slightlyoblique;noteumbilicalplate(up)in6.FromMaestrichtian,BeticCordillieras. 8-10 Randomlyobliquesections.MaestrichtianBeticCordillieras. 11-12 Lateralandbasalviewsofisolatedspecimens;Gowda'smaterialfromVilagudilimestone,Ariyalurgroup,SouthIndia;Maestrichtian. 13-17 Seriesofsectionsperpendiculartoshellcoilingaxes,from13nearesttoshellapexto17inshellbasis.Gowda'smaterial. 18-19 Subaxialsections,notquitecentered;Gowda'smaterial. Zitteliana,20,1993 12 Hottinger,L.&Caus,E.:Praestorrsellaroestae(Visser) Plate 218 SYSTEMATIC POSITION OF PRAESTORRSELLA 4. Byitsmodestsizeanditsmarginal,radialornamentationof ly specialised rotaliids with similar strucrural features, the ventral shell surface, P. roestae resembles a Trocholina. „Pseudorotalia"schaubiHottinger(1966),appearalreadyin Althoughtrocholinashavenosepta,itsumbilicalarchitecturc EarlySantoniantimes.ThesameistrueforRotalias.str.with admitsacanalSystemwithsimple,radialpassagesconnecting R.reicheliHottinger(1966)asanequallylargeandspecialized the main lumen with a network of umbilical canals and a species,whilepararotalias(withatruetoothplate;Hottinger wreathofradialgroovesnottransformedintoacavitySystem etal. 1991)appearwithPraestorrsella duringtheCampanian by subsequent shell layers (Hottinger 1976). The question timeinterval. arises, if the ventral, marginal ornament common to tro- There are two extant genera showing some remarkable cholinidsandPraestorrsellamayrevealaphylogeneticlinkin similarities with Praestorrsella: DiscorbinoidesSaidova, 1975 particular between Neotrocholina valdensis Reichf.l (1956), (type:D.subpatelliformisSaidova,1975)ischaracterizedbyan withaprimarycalcitic test,andPraestorrsella. On theother umbilical ornamentation with peripheral, radial grooves and hand,similarradial, marginalornamentationonventralshell umbilicalpiles(textfig.2).Theumbilicalpilcsareproducedby surfacesareknownastrueanalogiesinsuchunrelatedformsas markedlamellarinflationoftheimperforatefoliarwall.When Bolivinella, Annulopatellina. Angulodiscorbis and Glabatella superposed in successivewhorls,theyformcontinuous piles (see Loeblich & Tappan 1987). These Ornaments are a similartotheonesinPraestorrsella.Theumbilicushoweveris functionalfeatureindicatingplastogamicreproductioncycles notentirelycoveredbyfusedfolia.Thedorsalsideisevolute (seeLoeblich&Tappan1964=gamontogamiccycleinLeeet butcoveredwithfinepustulesobscuringthepatternproduced al. 1991). However,Praestorrsella shellswereneverfound in by the chamber sutures. The latter are strongly inclined plastogamicposition,ventralsurfaceagainstventralsurface,as backwards, while the umbilical chamber sutures are radial, it is occasionally seen in residues containing Bolivinella, again as in Praestorrsella. A specimen with missing ventral Glabratella orPatellina.Thus,we havetokeep in mind the chamberwalls(probablyresorbedduringplastogamy)figured combination of an umbilical canal System linked by radial byHOTTINGERetal. 1993,pl.148,fig.5,showsseptadisposed passagestothemaintubulärcavityoftheshellwithaventral inradialdirectionbelowtheventralwallandforkedtowards ornament indicating plastogamy as a feature common to the umbilical cavity. The fork indicates the double-walled TrocholinaandPraestorrsella. natureoftheseptumandthereforethepresenceofaseptalflap. ThepresenceofanumbilicalplateinPraestorrsellamayhint There is obviously a shallow dement closing off the main toaphylogenetic linkwiththegroupofLateCretaceousto chamberlumenfromtheumbilicalcavitiesandinterpretedhere PaleogenerotaliidsandinparticularwithStorrsella(Drooger as umbilical plate. In dorsal direction, above this dement, a 1960). Although documented only by drawings, this genus wide radial passage admits communication between main doubtlesslypossessesawelldevelopedumbilicalcanalSystem, chamber lumen and the umbilical cavities. This internal asingleinteriomarginaltomarginalaperture,umbilicalplates architecturcisalmostidenticalwiththeonedescribedherein and dorsal alar Chamber extensions. The existence of open Praestorrsellaroestae. intraseptalSpacesishighlyprobablesincetheventralsutures Conorbella Hofker, 1951 (type: Discorbina pulvinata aredeeplyfissuredandremainpartiallyopen. Brady, 1884) is less known as to its interior morphology. Lockhartia (Muller-Merz 1980)isdistinguishedbyfoliar However, theumbilical ornamentation is identical and there apertures present in Praestorrsella and missing in Storrsella. are heavy dorsal pustules much like those ofPraestorrsella Praestorrsella cannot bc a direct, Late Cretaceous predeces- roestae.Incontrasttothelatter,bothextantgeneramentioned sor of Paleocene Iockhartias because large, complex, high- herehaveevolutedorsalsides. Plate2 Praestorrsellaroestae(Visser).-Freespecimens,topotypesfromMaastricht(Limburg,Netherlands).SEMmicrographs.Scalebar0,1 mm. Fig.1 Dorsalview. Fig.2 Dorsalviewofyoungspecimen;notePerforationinultimate,slightlyinflatedChambers. Fig.3 Dorsalviewoferodedspecimen;Noteseptum(s)spiralingupwardstowardsshellapex. Fig.4 Obliqueventralview.Noteperipheralradialornamentinpenultimateshellwhorlcoalescingwithdorsal-peripheralchamberwallin ordertoproducehemiseptula(hs).Theventralsuturecorrespondingtotheseptum(s)cannotbedistinguishedfromotherradial furrows. Fig.5 Lateralview. Fig.6 Obliqueventralview,ultimatehalfwhorleroded.Note„empty"spaceoverexposedpreviouswhorlwheretheinteriomarginalforamen (f)leftnomarkoftheseptum(s)whiletheumbilicalplate(up)withitssingle,radialpassagetowardstheumbilicalcavities,closesoffthe chambercavity. Fig.7 Oblique-ventralviewofdamagedspecimen.Alltheventralandperipheralchamberwallsofthelastwhorlarebrokenaway.Note hemiseptulaatperiphery. Fig.8 DetailofFig.7showingumbilicalplate(up)andradialpassage(arrow)inchamberofpenultimateshellwhorlseenthroughagapinthe foliarwallbelongingtothischamberandcoveringpartoftheumbilicus. Fig.9 Peripheralviewshowingforamenininteriomarginalposition,partlyobstructedbycementcrystalscoatingtheinteriorwallsurfacesof allcavitiesintheshell.s:septum;hs:hemiseptulum. ptteliana,20,1993 Hottinger,L.&Caus,E.:Praestorrsellaroestae(Visser) Plate2 220 Fig.2A-C:Discorbinoidessp.- GulfofAqaba,offMarineBiologicalLaboratory,Elat,RedSea;150m depth.Cameralucidadrawings. A.Notquitecenteredaxialsectionmissingproloculusandcentralumbilicalpile. B.Sectionparalleltoshellbase.Noterecliningseptaindorsalandradialseptainventralpartofthe shell.Lowumbilicalplates(up)appearinsectionas„Shoulders",thegapberweenthemcorrespondsto theradialpassages. C.Sectioninaplanedefinedbythepenpheryofthelastwhorl.Dorsalpartofshellremoved,ventral partobservedanddrawnbytransparency.Notelargesinglepilescrowningeachfolium.Radialpassage bykeepingopenradialfurrowbetweenneighbouringpileswhencoveredbysubsequentwhorl. CONCLUSION 5. P. roestae, as described above, shows general similarities, Thedifferenceinchamberarrangementonthedorsalsideof namely1.atrochospirallycoiled,chamberedshellofsmallsize, the shell, involute in Praestorrsella and evolute in all other 2.indicationsofplastogamicreproductionbyitsventral,radial, generaofthefamilyGlabratellidaejustifiesthemaintenanceof ornamentational grooves independant of or in addition to the particular genus Praestorrsella with its type species P. suturalpositions,3.dense,heavyornamentationonthedorsal roestae. Accordingly, the stratigraphic ränge ofthe family is side,exceptionalforshellsofsuchsmallsize,and4.thegroup extendedbyitsfirstappearancealreadyintheLateCretaceous ofpilesfillingthenarrowumbilicalspace,withrepresentative Campanian stage (compare Loeblich & Tappan 1987, De- genera of the family Glabratellidae. In addition, there is a crouez1989).Astothehistoryofplastogamicreproduction, striking similarity of the internal morphology of the shell Praestorrsella apparently narrows the time gap between berweenP. roestaeandatleastonespeciesofDiscorbinoides. possibleEarlyCretaceoustrocholinidplastogamontsandthe Therefore,thegenusPraestorrsellaGowda,1978istransferred EarlyTertiaryones. here from the rotaliid subfamily Rotaliinae to the family Glabratellidae. REFERENCES Azema,J.,Foucault,A.,Fourcade, E., Garcia-Hernandez, M., France.-UtrechtMicropaleont.Bull.,33:1-32;62figs.,12tab., GONZALES-DONOSO, J., LlNARES, A., LlNARES, D., LOPEZ- 5pls.;Utrecht. dGealrJruirdaos,icAo.yC.C,rReitvaacsi,coP.daendlasVezroan,asJ.eAx.te(r1n9a79s):deLalsasmciocrrdoiflalceireass GallETmrie,mRp.AMr.ea&(PSoonust,hJC.eMnt.ra(1l98P3y)r:enCeoensi)a.ci-aNne-wMsala.stSrtircathitgir.a,n1o2f(t1h)e: Beticas. - MonographiaUniversidadGranada,83pp.,25figs., 1-17,3tab.;Berlin,Stuttgart. Caus,46E.p,lsR.o;dGersa,naDd.a&. 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