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• W2313331422 abstract "Gazd zicki . A . a nd We b b . P- N. 19 9 6 . Foramini fe ra from t he Pect en Co ng lo me rate ( Pliocene) o f Cockb urn Isl and. A nta rctic Peninsul a.J». A . Gaz dz ic ki (e d .) Pala eo nt ol o g ic al Resul ts o r the Pol ish Anta rc tic Expe d ition s . Pa rt If. - Palacont ol ogi« Poloni ca SS. 14 7-1 74 . T he Pect en Cong lo me rate wa s fi rst pr o po sed a nd de scribed by Andersson ( 1906) at a ty pe local it y on Cockbu rn Isl an d . a s ma ll isl and s itua ted be tween l am es Ross a nd Se ym our Isl an d s . An tarc tic Pe ni nsu la . T he na me or the fo rmation is taken fro m the b ival ve Chlatnvs audcrsson i ( Hennig, 191 0 ) w hic h occur s in ab unda nce at th e type loc al ity. In the first pu bl ic at ion on the turam ini lc ra recovered fro m th is uni t. Holl a nd ( 19 10) described and illu strated a fa u na o r X ge ne ra and II s pe c ies . Early in vest igat or s e m ployed muc ro pa lco n­ to log ic al a nd pa leocl ima tic dat a in assig ning eit her a Plioccne or Pl ei st occn c age to the tormatio n and pa leonto logi st s agreed th at th e Pecten Cong lomerate rep res e nte d an int e r­ g lac ia l or pre -g lac ia l environme nt. In the pr ese nt investig atio n of th e to ra miuite ra . the di ve rs ity ha s been augmented to 19 ge ne ra an d 24 spec ies . T he assemblage c o nta ins onl y c a lcareo us bent hic ta xa . Ag g lut in ated and plan kiic ta xa arc no t present. R ich assemblag e s o r mucro fuuna and m icro fau nu/ fl nra in the Pecten Cong lo merate provide a biot op e o f more th an 100 spec ies. Hi gh e nergy. coasta l mar in e e nv iro nm en ts w ith wa te r d epths not exce ed­ ing 50 me ter s are deduced fro m Io ra m inifera l a nd other palcon tol o g icul dat a . T he re is no e vide nce Io r th e presen ce o r thick gro un ded ice s heets o r ice she lves o ver thi s area d ur in g dep os itio n. a lt hou g h th e occ urre nce of seas o na l sea- ice ca nno t be di scounte d . T he Iora mi ­ ni feral a sse mb lage is correlate d w ith a lmo st ide ntica l Pli ocen e asse mb lag e s from the Wr igh t a nd Tayl or Valley s . a nd so uthern and wes tern Mr Murdo So und . and Lar sem ann H ills near Pryd z Ba y. Ea st Anta rctica. Di a tom s w hic h eo -occur w ith th e Cockburn Isl an d Ioru mi nifera indicate a n age o r 2.X- 2. 0 Ma (late Pl ioceu e ) a nd K/ A r radiome tric age s or 3 .65 and 2.8 Ma (l ate Pli occ nc ) were obtained trorn basalt s which re sp ect ive ly und e rli e and po ssib ly ov er lie the Pecten C o ng lo me ra te . Pal eo ntol og ical d a ta ind ic ate dcglac ia l/i n­ tcrglacia l condition s a t latitu de 64 S in th e Antarct ic Penins ula . an d support a rg um en ts ravori ng re lat ive ly mild po lar c li mate in many part s of An tarctica duri ng the Pli o cen e. K e y wo r d s : Foram inifera . pa lco eco log y, Pl iocen e . g lac ial-de gfacia l hi st o ry. An ta rc tic a . A ndr; «]Ga-;~ick i" @default.
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• W2313331422 date "1995-01-01" @default.
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• W2313331422 title "FORAMINIFERA FROM THE PECTEN CONGLOMERATE (PLIOCENE) OF COCKBURN ISLAND, ANTARCTIC PENINSULA" @default.
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