- Page 1 and 2: UTRECHT MICROPALEONTOLOGICAL BUllET
- Page 3 and 4: CONODONT BIOSTRATIGRAPHY OF THE UPP
- Page 5 and 6: 11.2.4.6. 11.2.4.7. 11.2.4.8. The P
- Page 7 and 8: This paper forms part of the author
- Page 9: The Cambrian-Ordovician sequence co
- Page 13 and 14: 1.2.1.2. Type-locality and type-sec
- Page 15 and 16: Locolity 2 _S 0- Fig. 8 The Kopings
- Page 17 and 18: Horns Udde Formation - Bruddesta --
- Page 19 and 20: Figure 11 summarizes the biozonatio
- Page 21 and 22: Ordovician limestones of Sweden (19
- Page 23 and 24: Ljthostratigraphic Lithostratlunits
- Page 25 and 26: formities in the rock-sections. By
- Page 27 and 28: The highly discontinuous character
- Page 29 and 30: Type-locality: Kopingsklint, sectio
- Page 31 and 32: Type-stratum: The limestone bed in
- Page 33 and 34: section 6. Paracordylodus gracilis
- Page 35 and 36: II.2.4.15. The Prioniodus crassulus
- Page 37 and 38: 11.2.4.18. The Drepanoistodus force
- Page 39 and 40: BIOSTRATIGRAPHIC AND CHRONOSTRATIGR
- Page 41 and 42: norvegicum and Bryograptus kjeruifi
- Page 43 and 44: Lithostratigraphic classification u
- Page 45 and 46: Kk2 near Horns Udde (see locality 2
- Page 47 and 48: III,3. CORRELATION WITH LINDSTROM'S
- Page 49 and 50: navis/P.crassulus Zone (figs. 15 an
- Page 51 and 52: fig. 19 Sergeeva's conodont zones a
- Page 53 and 54: found on bland, and in fig. 19 a bi
- Page 55 and 56: Oistod;;.s-l~;;;olatus/P;i~niod;'s
- Page 57 and 58: IV.I. INTRODUCTION Wherever possibl
- Page 59 and 60: each the cusp. Where the depression
- Page 61 and 62:
d) The denticulation. Sometimes the
- Page 63 and 64:
Udde from member Dh 1 up to the top
- Page 65 and 66:
teristic and Pander's drawing is ve
- Page 67 and 68:
The oistodiform elements are highly
- Page 69 and 70:
Drepanoistodus inconstans (LINDSTRO
- Page 71 and 72:
Drepanodus amoenus and Oistodus par
- Page 73 and 74:
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 127 and 128:
Names of conodont elements. ac acod