Zemes un vides zinātnes Earth and Environment Sciences - Latvijas ...
Zemes un vides zinātnes Earth and Environment Sciences - Latvijas ... Zemes un vides zinātnes Earth and Environment Sciences - Latvijas ...
138 ADVANCES IN PALAEOICHTHYOLOGY Fig. 7. Poracanthodes sulcatus sp. nov. SEM micrographs of scales (A-B), crown views, anterior upwards, and thin section photos (C-J). A, holotype, LIGG 25-A-2613; B, LIGG 25-A- 2614; C-F, vertical longitudinal section of scale. Thin section 3776. C, general view; D, detail of the anterior crown part and base apex at higher magnification; E, magnified detail of the posterior crown part and base; F, detail of scale primordium at higher magnification; G-J, vertical transverse section of scale. Thin section 3790. G, general view; H, the right part of crown at higher magnification; I, the left part of crown and the adjacent base portion; J, detail of the base apex at higher magnification. Lūžņi-4 borehole, depth 176.5 m. Přidoli, Jūra Regional Stage, Lūžņi Beds of the Targale Formation. Abbreviations: arcpc, arcade pore canal, avc, ascending vascular canal, b, bone, d, dentine, oc, osteocyte cavity, pc, superficial pore canal, rpc, radial pore canal, rvc, radial vascular canal, sf, Sharpey’s fibre traces. Scale bars: 0.1 mm. to open on the surface. The arcade pore canals (Fig. 7 H-I) are just as wide as the radial canals and connect the latter and superficial ones to form the complicated net piercing the crown tissue. The high-pyramidal base is composed of densely lamellar cellular bone incorporating varying numbers of osteocytes and pierced by long traces of Shapey’s fibres. The osteocytes are densest in the apex of the pyramid, where they are largest and
J. Valiukevičius. Silurian acanthodians from Lūžņi-4 139 most clearly oriented along the almost horizontal growth lines, transforming into a Stranggewebe-like tissue(Fig. 7 E, F, J). Remarks. This punctatiform Poracanthodes is closestly related to P. punctatus Brotzen discovered in many regions (Brotzen 1934; Lehman 1937; Gross 1947, 1956, 1971; Märss 1986; Valiukevicius 1998, 2003 a; Burrow et al. 1999; Vergoossen 1999 a, b, c; 2000; Burrow 2003). From typical P. punctatus it differs in having an antero-median sulcus, random arrangement of pores on crowns, and winding “vermiculate” oblique superficial pore canals seen through the thin transparent outer layer in the posterior crown part. The histological microstructure is generally uniform with the scales of P. punctatus. Poracanthodes marssae sp. nov. Fig. 8 A-E 1986 Gomphonchus hoppei (Gross); Märss, pl. 29, fig. 7. 2003 c Gomphonchus boekschoteni Vergoossen; Valiukevicius, p. 51. Etymology. In honour of Dr T. Märss (Tallinn), the first discoverer of scales. Holotype. LIGG 25-A-2559, flank scale (Fig. 8 A). Type horizon. Venzava Beds of the Targale Formation, Pridoli, Upper Silurian. Range. Targale Formation and its Estonian equivalent. Material. 6 scales. Diagnosis. Punctatiform Poracanthodes having scales with smooth, flat, pear-shaped crowns with a long, narrow posterior spine-like corner; symmetrical lateral projections in crowns placed at the beginning of its narrowing; very small pores visible on the posteriormost crown part; scale bases deep, protruding beyond crowns laterally and far anteriorly; necks of medium height and linearly porose on all faces; sharp keel on the posterior neck mirroring the crown shape. Scale crowns are composed of acellular mesodentine or dentine, and durodentine; ascending canals with rare branches; branches of radial canals extend down to the base; one? radial pore canal with few superficial pore openings running back from the scale primordium; high-pyramidal base is composed of dense, thin-lamellar cellular bone. Description. Morphology. Scales are of medium to large size (crown length is 0.34- 0.81 mm). Crown is smooth, flat, without inclination, pear-shaped, consisting of a rhomboidal main plate and very narrow, spine-like posterior part that may be as long as the main plate (Fig. 8 A). Two symmetrical lateral projections of triangular form occur in crowns of some scales at the place where the prominent narrowing of the crown begins (Fig. 8 C, see alo Märss, pl. 29, fig. 7). Crowns of most scales have a shallow medial concavity extending almost the entire length. A few ?linearly placed small pores, visible only at high magnification, open centrally on the posteriormost crown part (Fig. 8 B). Very deep rhomboidal bases protrude beyond crowns laterally and far anteriorly. The base is always deepest in advance of the crown. The base/neck junction is outlined by a clear anterior rim. Necks are well developed, of medium height and porose on all sides (Fig. 8 A). Pores are large, forming linear rows. A sharp vertical keel on the
- Page 87 and 88: O.A. Lebedev. A new tetrapod from R
- Page 89 and 90: O.A. Lebedev. A new tetrapod from R
- Page 91 and 92: O.A. Lebedev. A new tetrapod from R
- Page 93 and 94: O.A. Lebedev. A new tetrapod from R
- Page 95 and 96: O.A. Lebedev. A new tetrapod from R
- Page 97 and 98: O.A. Lebedev. A new tetrapod from R
- Page 99 and 100: ACTA UNIVERSITATIS LATVIENSIS, 2004
- Page 101 and 102: E. Lukševičs, I. Zupiņš. Sedime
- Page 103 and 104: E. Lukševičs, I. Zupiņš. Sedime
- Page 105 and 106: E. Lukševičs, I. Zupiņš. Sedime
- Page 107 and 108: E. Lukševičs, I. Zupiņš. Sedime
- Page 109 and 110: E. Lukševičs, I. Zupiņš. Sedime
- Page 111 and 112: E. Lukševičs, I. Zupiņš. Sedime
- Page 113 and 114: E. Lukševičs, I. Zupiņš. Sedime
- Page 115 and 116: E. Lukševičs, I. Zupiņš. Sedime
- Page 117 and 118: E. Lukševičs, I. Zupiņš. Sedime
- Page 119 and 120: E. Lukševičs, I. Zupiņš. Sedime
- Page 121 and 122: J. Valiukevičius. Silurian acantho
- Page 123 and 124: J. Valiukevičius. Silurian acantho
- Page 125 and 126: J. Valiukevičius. Silurian acantho
- Page 127 and 128: J. Valiukevičius. Silurian acantho
- Page 129 and 130: J. Valiukevičius. Silurian acantho
- Page 131 and 132: J. Valiukevičius. Silurian acantho
- Page 133 and 134: J. Valiukevičius. Silurian acantho
- Page 135 and 136: J. Valiukevičius. Silurian acantho
- Page 137: J. Valiukevičius. Silurian acantho
- Page 141 and 142: J. Valiukevičius. Silurian acantho
- Page 143 and 144: J. Valiukevičius. Silurian acantho
- Page 145 and 146: J. Valiukevičius. Silurian acantho
- Page 147 and 148: J. Valiukevičius. Silurian acantho
- Page 149 and 150: V. Pernegre, V. Dupret. Biostratigr
- Page 151 and 152: V. Pernegre, V. Dupret. Biostratigr
- Page 153 and 154: V. Pernegre, V. Dupret. Biostratigr
- Page 155 and 156: V. Pernegre, V. Dupret. Biostratigr
- Page 157 and 158: V. Pernegre, V. Dupret. Biostratigr
- Page 159 and 160: Ž. Žigaite. New telodont from Tuv
- Page 161 and 162: Ž. Žigaite. New telodont from Tuv
- Page 163 and 164: Ž. Žigaite. New telodont from Tuv
- Page 165 and 166: Ž. Žigaite. New telodont from Tuv
138<br />
ADVANCES IN PALAEOICHTHYOLOGY<br />
Fig. 7. Poracanthodes sulcatus sp. nov. SEM micrographs of scales (A-B), crown views, anterior<br />
upwards, <strong>and</strong> thin section photos (C-J). A, holotype, LIGG 25-A-2613; B, LIGG 25-A-<br />
2614; C-F, vertical longitudinal section of scale. Thin section 3776. C, general view; D, detail<br />
of the anterior crown part <strong>and</strong> base apex at higher magnification; E, magnified detail of the<br />
posterior crown part <strong>and</strong> base; F, detail of scale primordium at higher magnification; G-J, vertical<br />
transverse section of scale. Thin section 3790. G, general view; H, the right part of crown at<br />
higher magnification; I, the left part of crown <strong>and</strong> the adjacent base portion; J, detail of the base<br />
apex at higher magnification. Lūžņi-4 borehole, depth 176.5 m. Přidoli, Jūra Regional Stage,<br />
Lūžņi Beds of the Targale Formation. Abbreviations: arcpc, arcade pore canal, avc, ascending<br />
vascular canal, b, bone, d, dentine, oc, osteocyte cavity, pc, superficial pore canal, rpc, radial<br />
pore canal, rvc, radial vascular canal, sf, Sharpey’s fibre traces. Scale bars: 0.1 mm.<br />
to open on the surface. The arcade pore canals (Fig. 7 H-I) are just as wide as the radial<br />
canals <strong>and</strong> connect the latter <strong>and</strong> superficial ones to form the complicated net piercing<br />
the crown tissue. The high-pyramidal base is composed of densely lamellar cellular<br />
bone incorporating varying numbers of osteocytes <strong>and</strong> pierced by long traces of Shapey’s<br />
fibres. The osteocytes are densest in the apex of the pyramid, where they are largest <strong>and</strong>