• Nie Znaleziono Wyników

Problemy stratygrafii trzeciorzędu w świetle badań palinologicznych

N/A
N/A
Protected

Academic year: 2021

Share "Problemy stratygrafii trzeciorzędu w świetle badań palinologicznych"

Copied!
5
0
0

Pełen tekst

(1)
(2)
(3)
(4)
(5)

in Mltte1europa. Rev. Palaeobot. and IPaolynol. 2, s. 147-16c. Amsterdam 1967.

2. BlL"elie G. - Zur mi·krot1oristiEchen Schichoten-gliederung im rheiJD!echen BraunkohlE!lll'revier. For1lschr. Geol. RedJndd. u. West;f8!l HI,

s.

35-<102,

Krefeld 1968.

3. K r 'll t

z

s ch W. - Einige Fragen der weiteren

spoo:en:palaantolog:ischen Erfol'Sch'Wlg des Tertiars der Lausiltz (i.w.S.). 1959.

4. K rut.z

s

c h W. - stratig:raphische und klimatoo-J.ogiscbe Bemerktmgan

zu

des Lausitzer und m.it-teldeuflschan TertUirfJ.oren. PaUionJt,

Z.

34 (1) s.

15---d.6, 1960.

5. Kr-utz8ch W. - Der Florenwechsel im Altter-tHir MiJtteleuropas aut GI'UIIld von sporen,palaon-tollogische UntersuchUlllgel1. Abh. :lleIlltr. geo!..

lost.,

H. '10,

s.

17-37. Berlin '1967.

SUMMARY

The aIfticle gives new method of using pollen gradns atnd spores to determine stratigraphy of the Upper Tertiary :brackJsh and oo:ntinenJtal desposits, w<Xl"ked out in Berlin by W. Krutzsch. The method under CCCDSideraili'Oln has been 9timulated by the

re-sults

of macrofloristk: ,study, obtained by D. H. Mai, which prove a cyolic changes of climate art 'the Youn-ger Tertiary time. On this buis and on his own

observations s.howmg !that rare forms of poLlen graiIlS of entomqphilous plants, found during the analyses, are impol'/tant climattc mdices, W. Krutzsch emphasized a Illecessity of makimg qualdltative

analy-sjs and of determdm.i:ng the highe&,t possible amount of microfossiils. He also proposed 8 graphical

pre-sentation ott gl'0U,Il9 af pollen forma that appear un-der similar cLimatic

con.di:tians.

Thi'll

new

qualdJlati-ve-quantitartive method will no doubt heu.p ;In ma-king ocorrelatioQS of the :indiv:iduaiJ. micro!loriSltic. horiZOlDS in ;the Middle Europe area, and ID deter-mining theiT position :!in the stratigraphical table.

6. ·Krutzsch W., Majewskd. J. - iZur

Metho-cUk

der pollenstratigraphlschen Zonenglieden.mg

im JU1l8tenitu' Mi1lteleuropas. Abh. ~nItr.

gB9l

IJDst.

H. 10, s. 83-98, Berlilll 1967.

7. M a:l. D. H. - .Die FlorenzohneaJ., der F1l.orenwech-sel und die Vorstellungen' liber den Klimaab1.auf

im JungtertUir der DeUJtschen Demokratischen Republik. Abh.

zentr.

geol. Dnst. H. IQ,

s.

55-81. Berlin 1967.

8. P flu g H. D. - Zur AltersfQlge und FaziC!:l~ie­ derung mJ.tteleuropii'ischer (insbesonders hessis-cher) Bra-u:nkohlen.. Not1zbla.'IIt hess. L.-Amt. Bc-denforsch. Bd. 85, s. 162-178. Wiesbadcn 1957.

9. P f iI. ug H. D. - Bemerlkungen zur Sporan&trati-graphlie im hoheren Ter.tiiir. Z. delllf.SlCh. geol. Ges. Bd. 115, t. 1, s. 69-76. Hann,over 1963.

PE3IOME

B CTaTbe paooMaTpHBaercJt' HOBhDi: MeTO~

HCrrDnb3IJ-BaHHJt mUIbIU>1 H cnop ~JUl CTINl-TKr.Paq,K'lecKod,)"pac-'IJIeHelDUI CDnQHOBaTOBoAHbJX H KOH'1'HHeH'l'aJIbHblX BepXHeTPe'1'JAH1:dX O'1'JI02IreHrui:, Pa3pa6oTama,m B Bep-JIHBe R. Kp~eI4. MhrcJIh C()3ABIDUI TaxlOl'O MeTO~a

nOJtBHJIaCb B CBJt3K C pesyJIhTCl"l'aMJ! Kaxpoq)JIopHCTH~

'IecKHX troCJle~KA. DOJIy<leHHbEWI ,D;. X. MaAeM

H Y'Ka3bIBaro~ Ha ~K:K.llK'Iec~ KOJIooaHHR KJIH-MaTa ·B n03W1~oe BpeIIR. STK ~8HHbret a TaK:-2Ke co6c'l'BeHHble HIl6JIIO~eHHJt B. Kp~a, ,l\QKa3bl-BalOll{He, ':1'1'0 pe,lllltHe nblJIbqeBLIe q,oPMhI JtBJIRIOTCR BaJEHI:oIMH K.JmM8.'l'H'iecJmIMH DOKa3aTeJImiIt, 38CTaBHJIH 06.pa'1'Wl'l> oco6eHm>e BBHMaBHe Ha 'l'U(QTeJIhHLIfl lta'le-CTlBeHHhDi aHaJIH3 B03MOlKHO HaH6c:mLmero JD>JI'H'Iec'l'BO M:H'lqlIOOJt8MeHenOCTeft. B. Kp~w IIpe,!{JJIOlKHJI TlUOKe

cPopMy rpa~ l£306palKeBHJl IILI.lIL~EllIa1X

cPoPM

IlIO rpymIaM, «JPe~eJIHIOIQJtK cxo~ K:.JIHMa'1'JAec~ YCJIOBHH. 3'l'1Yr HOOhDi: KB.'IecTBeHlIO-«toJl'H'lec'l'BeHHLIli KeTOA lJ03BOJIIle'l' IHa.A61ITLCJt, 'Iro

c ero

[l()MO~ MiOJiC~ HO fiYAe'l' rrpoaecTH K~ 0'l'Aem.m.IX MmtPO-q,JI.OpHC'l'.K'ft!CK'HX ropH30HT0B Ha '.l"8P.PJt'.l'

Ueu-T.P8JIJ;oIHOft EBpoIIhI H ycTaB.'OBHTL me: no3HQMllO B CTP8--mrpacPIAeoJroft '1'86~e.

Cytaty

Powiązane dokumenty

In addition to that in the Whitecliff Chert and Bindon Sandstone in west Dorset, Tresise (1961) referred to some of the siliceously cemented beds in the Foxmould in the

The more southerly of the fallen blocks on the beach [SY 8032 to 8646] shows the highest bed of the White Nothe Member to be a massive, dense, highly bioturbated calcarenite

The Upper Turonian Großberg Formation of the Regensburg area (Danubian Cretaceous Group, Bavaria, southern Ger- many) has a mean thickness of 20–25 m and consists of sandy

A high-resolution stratigraphic calibration of the upper Lower (upper Mantelliceras dixoni Zone) and lower Middle Cenomanian (Cunningtoniceras inerme Zone and lower

Christensen (1995) dis tin guished three chronospecies within the lin eage of B. mi nor II and B. The lat ter was in cluded in the syn on ymy of B. mi nor from the Mid dle

ABSTRACT: The Czorsztyn succession in the Pieniny Klip.pen Belt of Poland comprises, at the RogoZa kliWes near Rogotnik, the RogoZnik Coquina Member (Lower

The earliest trace fossils' from the sediments orfthe uppermost Vendian (Brzegi Shale Fm.) are represented by exichnial burro, w casts (Gordia sp.) and epichnial

The di a tom suc ces sions at Komorniki and Domuraty are sim i lar in the abun dance of plank tonic spe cies of Stephanodiscus and Aulacoseira, as well as in the