iLITlDRATURA
1. B e:Hekls W: J. ~ Osado<:7myje .fOll."mad j
liw..
Iogiczes!k'l.~ .k.omp1eksy paleogena if neogena Jui:-noj! ~, Tr.
mst.
CHeol, wy!p. 3. ViImus,1986.
2. C i UI k E. - Schema,!;y titostra'tyerafilc'me
trze-tclOrqdu. Niiu PolSkiego. ~L .geol.,
uno,
nr 4.~. iD y)or S. - Seria pomaDaka w Po1sce zaehod-n1ej. .Ibldem, 1970, nr
4-4.' Fursel!llllto A. W., Fursen.ik'o K. B. - Fo-Irmmnlifiery Wlierelmiiego eocena Bl.elol'U88i i i'!:h ~rsU~~je ,ZBlCzeni·je. Pal~1. i stra-,bigral BS9R,
e.
111. Miilllllt, 1981.5. G ri g t a, liis A. A. - 0 wozra"Stle 1 nrlikrClfauo:e pogram.i.eznych mde'idu mieitom i paleogendm
slo-jew w Jumoj Priba*lk:le. W sb. Gra,niea
mielo-twycb i tri6biCZllych ot~temj. Mieid. 9Ieol Ko • •
.:xxt
$k!slja, ddd. scIW. gieo:logow, pro1:jI.. 5 M, U'9I60.8. GI1'JlILalb A., B8'Uakh W., Katd:nas W. . - StratlgrafUa paIleogenow"ch otIozenij
Pr£bal-'tlk'f.. lz'w. AN SSSR. S!ler. ei~. Jll' 3. M'oskrw>a',
'1971.
7. Reer O. - Mfucene'balMi8che FIlora.. K6ailCsberg,
1869.
8. IK 0 en! eo'!) A. - ReviSion der MdIluekenlaUllUl IdEfs 86lIDlendfschen Tel"t!Iers. A'bbandl. Z. 8eol. lSipezialkarte v. PreUIIIs., Brei. 10, H. 7. Ber'I'i,n, 1894. ;
9. MI8i'kail"enko D. E. - Pereiblad s'WatYbRtkz-nom ~oZen* lattorMobo ja'l'US8. NimylC'zczyny. meo1.
2lE'D.,
t. 18, wyfp. 1., 1.10. M;a"er K. - Die F8'Uina des madnen SMld-I5telnes' ~ KleVnkubren beli.-K~erg. Viertel-jabr. Naot.
Gesem.
ZUJr'.i!ch, Bd. 6, .11881.V 11. M It r IZ e C Mo - Zary.s hu1dowy geoloigieznej u-rtwar6w tzzeciorz~O\VY'Ch i c'Z'Wa'rtOl."Z~doWYICh rN
Irejonde Zatdki Puddej. Prz. geo!. 1971, nr 12. 12. N
oeH
i -lIIg F. D. - Die !'aWla dessalmllJa,ndi-lIChen Tertier8. Bd. 1--111~ Abbandl. Z. goot Spe-tzidkarie
v.
~euss., Bd. 8, H. 31-14, Berllin, 18811.13. Paesen:dOlrfe!1' E., Zab~oC'ki J. - 0 trze-lCiorz~wych 1 czwar!fm'Iz~wych \ttworaeh
brze-p Baltydru pomfQdzy W~ WBiIl
a
Jubrz~illG6rtl- Boezn. Po1. Tow. Gd., 194"6, z. 3.
14. IPawlowBk'f S. ~ Cbara-k!teryBi;yoka
modolo-«ficma wybrzem
pols'k!ielgo. Po7m.an, 192'2. 1~.· p'o'f:aryska K:, Locker S. - Lesorganis-mes pIlandonique.! 1'00cette ~eur de Slem1eJi. ~e Orientaline. Rev. de MiCro'pa~~nIt., 1972, . ~·.5.
t; HS. .P azdiro Z. - BtIdIowa geologflCzna· regionu
gda6-sldego. Roczn. Po'!. 'fuw. Geol., 1980, z. 4. 1'1. Rudo'W'&lIii S. - Geololia kllfu K~Y'
Swa-.. lr2ewa1de). Jb{dem., 1'985, om 2..
18. Sa;tmI:solliow&C'~ J. -
Uber
d:as Quartllr UIIld !den P'nt.ergrund fm ~hen Su:dba1t1culm nach . rri~u\n.'gen in. Juraifa uod Kar'W'ia. Geol.. Foren. Bel. 60, R. 4. S~lm, 1938.
IQ.. Wehihoh E. -
Uber
die Gtiecienmg des AlJ:tteritlars im Wesmchen MeklenbUJr'g. Sanderd'!'. a. d.. .. ~ .Beritclbte d. geol. Gesetl. Bd. TII,. .. H. 2/tJ, BeriUn., 19158.
2O.Wof.ny ·E. - stratygrafia oligocen-u PoJi.9ki
Za-' ;ebIodnie'j,
na
~ m9krofalmY. Kwarl. geo1.,1982, 114" 1;
M. 'Wi () Z 'Il Y E. - Eocen z Siemienia' kolo Pa!'CZewa,. lIMdem~ 1'966, .nl" 3.
22. 'ZleHcl9ka'h W. A., l(!·ulHscben'ko B.G.,
-:Ma'tt a ren.ko D. E., 901"0 he ha n E. A. lPa'leon'tologjczelSldJ sprawocznilk. IGjew, 1988.
SUMMARY
lAtholOgy am stra;Ugr-BlPhy of the Tertiary' firorQ ·the JaBtrzQbia G6ra a-nd IPu.lck areas, nortthenn PolaQd;
are d'i'8Cusseci on the be&is of core ma-teria,]s,.
ere.,
taceous aulJlstralta i.nJcIUJde Lower Turoniainsiltsltones wi:th 1 MCe1'amus labiatus Se h lot h., AnomaJina be1'theUni K ell er, Ling~logatlelineUa gWba.a (B rot z e ill), a'nd o'thers, and Cenom8lllian quartz--4leuoondte lSands rih n.umerous ,i,nooenunide andbelemnites. . .
Boreholes have provided almost oo.nIi;inUOwt core! of the Eorce.ne, Oligocene an-d Miocene. In.·the Eocene.; -Olf.gocene eeguenJce, 5 series8!l."e dIstinguished. TbIl'ee lamest of these series &re pa.leontologJ.cal1y dalted
and ~
O!f
i!reat .impar!la·nce as they l'epre&en.t a new. example of ·the ~·u.rrerree of these JIltbo$traofligra.phdiC'al ooLts.m
:sl-n.gJ.e ver:tkal;pro:rue.
The olldest serile's, >COmmonly 2.0-<3.0 m th4ck, named herem the lower Mie.ro&zyoo series, oonsists of dElP'O'Si1f:s of 8he~w-water tnail'.me fa'Cies, euch Ba
marly sll't9tooeB with gla'Uoonite, phOSjphordltes, quartz:
gravels, a·nd lumps of iron SUiIpmdes. MicrClfaunal assemblqe. indilCaitdlVe of the Upper Eocene ale,
campr1se!l such forms as: Cibicides auzakenBiB B y k.,
Lenticulina dtmorfa T Cll t k., and U vigerina co,teUata
Mot. MaICIrofauna i.nddIca.tmg the Barihonian age of ~bese deposits lc.cIUdes IPe!k!lcY'Poci, Vene1'icanlta ditle1"-gem praeculta (iK.lu6eh·n!fikov), a·nd other forms.
The next series, a few meter thdck and named
he:retn
.the . upper Mier.oszyoo series, consi. of l'e-ma!rlkabty homogeneouB clayey, decalcified S!ilhstones. TheSe Btre:ta are ilnddaal\lWe CIf sedJmen.tatlonunder'
more qwet conditbions tha.n those ooder whi-ch the lower Mieroszyno series was deposited.Pa'ly.nolOglcaf
s.tUldJes show the la.test Upper Eoicene age of 'these.strata.. .
The overJ.ylng s1lrata, represented. by a series
oIt green sam
and sandy qwwt"L-tg,ltaUlCOllite sf!1jg ·with amber and &iIl4tle pbosphorites, a few meter thdlC"k, are dated on the basilS of remarkably il"1cher faunal assemblage. The assemblage tCO~Js-es such formsas: Cardita latesulcata N y s t., BalanophllUa
aubctl-liMrtca P1i;ftll ipp, Ct/prina cl. pero'VaU,
Koeneo,
Panopea gastaldi M iI.c h., 180CQrdia muUtBulcata N yla t., Ce1'atobulimma contTaria R e'lllltiS, Lentipecten comeus . . (50 w e r by). a·nd others, . i·nQLcoaUve 01. the La-ttorfiJan age. Accordi·n.g.·to the !lIiOIIDienclaltul'e propo,sed herein, the series is named the Poiczyno ser.l.es.
DeposdtI;s of a 9\,lIocessi.'ve sedimentary cY'CJ.e, w'htleh presumably is of the Middle Oligocene age, at'e l'etprelle.nJteid by ooifoml, homogeneou!s Stet'ies' of ma.1"Ii'1le, grey-green., Q.Uta1"itz...gla1.M:onite sand&, -devoid o£ 'fauna!: record. The serfJes is a flew meter' th;l.cik, on the:· average.
The yoooge6t link of the Palaeogi!D.e f·rom
the
area lnquestion ja re..oresented by deposits .w'bkh originatbeci in braddsh or marshy enviro.nment. These depooits are represented. by eerieSt of dBrlt-l.rey -clayey alUs, hori!'wn:flalllq lambnated ·wd.lth quu·bz saon~t These silts y.ield· carbonJ:zed Plat rema!ns an<l in-numerous gTaiDs of glauoonite. The sedes is thj·n end attaias a few metersm
thddlmess, on the'average. .
Top pa4'IfB of the prof.lle in question aa-e l'epre-serrted· by depos£t& of the late Tertiary - N'eogene
-whd'Ch origdnarted in land-looked, freSth-lWateL' baslm..· TbiS series, a few .tens of meters in thda1mess-, comlpIlises quartz, micaceDU& thi.nJy-lbed'Cied sands and saDdy: snts wdth admildUd"e of cail'lboni~edI p1a·nt l'II!'lDll'lrul. Upper part of .tlWs .ser.ie6, yie1di·ng .. thln beds of MOWln coa:Js., well-ex.posed In Chlapowo a.n4 Rozewde cll«s. has been. assigned
to
the Lower. Miocene on the bas18 of iden'ti!fJ.~ations of· flowremaLn.&. . ,_ .