UTRECHT MICROPALEONTOLOGICAL BUllETINS

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Names of conodont elements. ac acodiform oz ozar kodinaform ar arcuatiform pac paracordylodiform cd cordylodiform pp pipaform dr drepanodiform pra prioniodinaform dt deltaform pri prioniodiform el elongatiform rd roundyaform e.s erect scandodiform sc scandodiform fl falodiform sp sculponeaform gt gothodiform se suberectiform gr graciliform sn sannemannula ir irregulariform sip scandodiforml p altodiform lr longiramiform trc trichonodellaform mr multiramiform trg triangulariform oep oepikodiform tit tetraprioniodiforml o/f oisto diforml falodiform trapezognathiform ois oistodiform
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UTRECHT MICROPALEONTOLOGICAL BUllET
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CONODONT BIOSTRATIGRAPHY OF THE UPP
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11.2.4.6. 11.2.4.7. 11.2.4.8. The P
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This paper forms part of the author
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The Cambrian-Ordovician sequence co
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-E Section C Section b w Section a
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1.2.1.2. Type-locality and type-sec
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Locolity 2 _S 0- Fig. 8 The Kopings
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Horns Udde Formation - Bruddesta --
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Figure 11 summarizes the biozonatio
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Ordovician limestones of Sweden (19
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Ljthostratigraphic Lithostratlunits
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formities in the rock-sections. By
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The highly discontinuous character
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Type-locality: Kopingsklint, sectio
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Type-stratum: The limestone bed in
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section 6. Paracordylodus gracilis
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II.2.4.15. The Prioniodus crassulus
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11.2.4.18. The Drepanoistodus force
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BIOSTRATIGRAPHIC AND CHRONOSTRATIGR
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norvegicum and Bryograptus kjeruifi
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Lithostratigraphic classification u
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Kk2 near Horns Udde (see locality 2
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III,3. CORRELATION WITH LINDSTROM'S
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navis/P.crassulus Zone (figs. 15 an
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fig. 19 Sergeeva's conodont zones a
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found on bland, and in fig. 19 a bi
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Oistod;;.s-l~;;;olatus/P;i~niod;'s
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IV.I. INTRODUCTION Wherever possibl
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each the cusp. Where the depression
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d) The denticulation. Sometimes the
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Udde from member Dh 1 up to the top
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teristic and Pander's drawing is ve
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The oistodiform elements are highly
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Drepanoistodus inconstans (LINDSTRO
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Drepanodus amoenus and Oistodus par
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Regional occurrence: At Kopingsklin
Page 75 and 76: oistodiform element (PI. 7, figs. 7
Page 77 and 78: Genus Oistodus PANDER, emend. VAN W
Page 79 and 80: Regional occurrence: At Kopingsklin
Page 81 and 82: of Drepanodus arcuatus PANDER, emen
Page 83 and 84: Remarks: Throughout the Oland secti
Page 85 and 86: elements (after Trapezognathus LIND
Page 87 and 88: (LINDSTROM), emend. herein (see PI.
Page 89 and 90: conodonts" and the "complex conodon
Page 91 and 92: in member Ka- d 1 and Ka- d 2 of se
Page 93 and 94: Protopanderodus latus n. sp. (PI. 4
Page 95 and 96: Protopanderodus rectus (LINDSTROM),
Page 97 and 98: it is not thickened towards the rim
Page 99 and 100: flaring and opens to the least conv
Page 101 and 102: emend. herein (PI. 2, figs. 9, 10).
Page 103 and 104: 1961: Discontinuity surfaces in lim
Page 106: Figs. 1a and 1b Coelocerodontus bic
Page 110: Figs. 1~4 Drepanoistodus conulatus
Page 114: Figs. 1-7 Triangulodus brevi basis
Page 118: Figs. 1-4 Oelandodus elongatus (LIN
Page 121 and 122: ~~ Light green shale. tP}·('WJ Lig
Page 123: Names of conodont elements. ac acod
Page 128: I :g I I( Location of the samples T
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UTRECHT MICROPALEONTOLOGICAL BUllETINS

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