<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>0120-0283</journal-id>
<journal-title><![CDATA[Boletín de Geología]]></journal-title>
<abbrev-journal-title><![CDATA[bol.geol.]]></abbrev-journal-title>
<issn>0120-0283</issn>
<publisher>
<publisher-name><![CDATA[Universidad Industrial de Santander]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0120-02832009000200010</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[OCCURRENCE OF SELLITHYRIS SELLA (BRACHIOPODA) IN THE ROSABLANCA FORMATION, BOYACÁ-COLOMBIA]]></article-title>
<article-title xml:lang="es"><![CDATA[REGISTRO DE SELLITHYRIS SELLA (BRACHIOPODA) EN LA FORMACIÓN ROSABLANCA, BOYACÁ-COLOMBIA]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rojas-Briceño]]></surname>
<given-names><![CDATA[Alexis]]></given-names>
</name>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Patarroyo]]></surname>
<given-names><![CDATA[Pedro]]></given-names>
</name>
</contrib>
</contrib-group>
<aff id="A01">
<institution><![CDATA[,Departamento de Geociencias Universidad Nacional de Colombia ]]></institution>
<addr-line><![CDATA[Bogotá ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2009</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2009</year>
</pub-date>
<volume>31</volume>
<numero>2</numero>
<fpage>129</fpage>
<lpage>132</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0120-02832009000200010&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0120-02832009000200010&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0120-02832009000200010&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[The brachiopod shells discovered in the Rosablanca Formation from the Santa Sofia locality, NW of Villa de Leyva, Boyacá province, can be identified as Sellithyris sella (J. de C. Sowerby, 1823). The studied material shows characteristics features of this taxon including the loop wide, triangular with high-arched transverse band. This material was collected during a paleontological excursion with geology students. Sellithyris was previously reported from Zapatoca, Santander province by Dietrich (1938) and Karsten (1958).This new record documents its wide Late Valanginian-?Hauterivian distribution in Colombia (Uppermost Rosablanca Formation) and confirms the direct transatlantic connections with Western Europe.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Se describe la ocurrencia de Sellithyris sella (J. de C. Sowerby, 1823) en la Formación Rosablanca, proveniente del área de Santa Sofía, Departamento de Boyacá. El material estudiado comprende dos ejemplares completos y seis moldes internos colectados en una excursión con estudiantes de geología. El brquidium amplio, triangular y provisto de una banda transversa alta, preservado en uno de los moldes internos, es característico del taxón. Sellithyris ha sido registrado previamente en el área de Zapatoca, Departamento de Santander. Este nuevo registro indica su amplia distribución durante el Valanginiano Tardío-? Hauteriviano de Colombia y confirma las conexiones con Europa Occidental.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Sellithyris sella]]></kwd>
<kwd lng="en"><![CDATA[Rosablanca Formation]]></kwd>
<kwd lng="en"><![CDATA[Late Valanginian - ? Hauterivian]]></kwd>
<kwd lng="es"><![CDATA[Boyacá- Colombia]]></kwd>
<kwd lng="es"><![CDATA[Sellithyris sella]]></kwd>
<kwd lng="es"><![CDATA[Formación Rosablanca]]></kwd>
<kwd lng="es"><![CDATA[Valanginiano Tardío -? Hauteriviano]]></kwd>
<kwd lng="es"><![CDATA[Boyacá- Colombia]]></kwd>
</kwd-group>
</article-meta>
</front><body><![CDATA[   <font size="2" face="Verdana">      <p align="center"><font size="4"><b>OCCURRENCE OF SELLITHYRIS SELLA    <br> (BRACHIOPODA) IN THE ROSABLANCA    <br> FORMATION, BOYAC&Aacute;-COLOMBIA</b></font></p>      <p align="right"><b>Alexis Rojas-Brice&ntilde;o, Pedro Patarroyo</b></p> 	 <hr>      <p align="left">Departamento de Geociencias, Universidad Nacional de Colombia. A. A. 14490, Bogot&aacute;, Colombia    <br> <a href="mailto:arojasb@unal.edu.co">arojasb@unal.edu.co</a></p>  			     <p align="center"><font size="3"><b>ABSTRACT</b></font></p>      <p align="justify">The brachiopod shells discovered in the Rosablanca Formation from the Santa Sofia locality, NW of Villa de Leyva, Boyac&aacute; province, can be identified as <i>Sellithyris sella</i> (J. de C. Sowerby, 1823). The studied material shows characteristics features of this taxon including the loop wide, triangular with high-arched transverse band. This material was collected during a paleontological excursion with geology students. <i>Sellithyris</i> was previously reported from Zapatoca, Santander province by Dietrich (1938) and Karsten (1958).This new record documents its wide Late Valanginian-?Hauterivian distribution in Colombia (Uppermost Rosablanca Formation) and confirms the direct transatlantic connections with Western Europe.</p> 		     <p align="justify"><b>Key words: </b><i>Sellithyris sella</i>, Rosablanca Formation, Late Valanginian - ? Hauterivian, Boyac&aacute;- Colombia.</p> 		     ]]></body>
<body><![CDATA[<p align="center"><font size="3"><b>REGISTRO DE SELLITHYRIS SELLA (BRACHIOPODA) EN LA FORMACI&Oacute;N    <br> ROSABLANCA, BOYAC&Aacute;-COLOMBIA</b></font></p> 		     <p align="center"><font size="3"><b>RESUMEN</b></font></p> 	     <p align="justify">Se describe la ocurrencia de <i>Sellithyris sella</i> (J. de C. Sowerby, 1823) en la Formaci&oacute;n Rosablanca, proveniente del &aacute;rea de Santa Sof&iacute;a, Departamento de Boyac&aacute;. El material estudiado comprende dos ejemplares completos y seis moldes internos colectados en una excursi&oacute;n con estudiantes de geolog&iacute;a. El <i>brquidium</i> amplio, triangular y provisto de una banda transversa alta, preservado en uno de los moldes internos, es caracter&iacute;stico del tax&oacute;n. <i>Sellithyris</i> ha sido registrado previamente en el &aacute;rea de Zapatoca, Departamento de Santander. Este nuevo registro indica su amplia distribuci&oacute;n durante el Valanginiano Tard&iacute;o-? Hauteriviano de Colombia y confirma las conexiones con Europa Occidental..</p> 		 		    <p align="justify"><b>Palabras clave: </b><i>Sellithyris sella</i>, Formaci&oacute;n Rosablanca, Valanginiano Tard&iacute;o -? Hauteriviano, Boyac&aacute;- Colombia..</p>  <hr>      <p align="center"><font size="3"><b>INTRODUCCI&Oacute;N</b></font></p>      <p align="justify">The Colombian Cretaceous brachiopods include the terebratulids: <i>Arenaciarcula beaumonti</i> (d`Archaic) and <i>Gemmarcula</i> cf. <i>menardi</i> (Lamarck) deposited in the d`Orbigny Collection, and <i>Sellithyris sella</i> (J. de C. Sowerby, 1823), reported as <i>Terebratula Haueri</i> Karsten (1958) and <i>Terebratula sella</i> Dietrich (1938) from Zapatoca, Santander Province. This study documents the occurrence of Sellithyris sella (J. de C. Sowerby, 1823) in a stratigraphic section with good outcrop exposure of the Upper Rosablanca Formation from Santa Sofia (<a href="img/revistas/boge/v31n2/v31n2a10f1.jpg" target="_blank">FIGURE 1</a>), near of the &ldquo;la F&aacute;brica&rdquo; cave, Boyac&aacute; province. This genus is a low latitude Tethyan form (Sandy, 1997), and is present in Western Europe, North Africa, North America and Mexico (Sandy, 1997; Gaspard, 2005). Mance&ntilde;ido (2002) proposed that the occurrence of <i>Sellithyris</i> in Colombia and <i>Musculina</i> from northern? South America may suggest direct connections with Western Europe.</p>      <p align="center"><font size="3"><b>MATERIAL AND METHODS</b></font></p>      <p align="justify">The brachiopod shells were examined under a camera lucida and transverse serial sections were obtained by gridding one internal mold with 600 powder on glass plate. The dimensions (in mm): length dorsal valve (ldv), length (l), maximum width (mw), position of maximun width (pmw) and thicknes (t) were taken with a caliper. All material used for this report kept in the palaeontological collections in the Departamento de Geociencias, Universidad Nacional de Colombia, Bogot&aacute;.</p>      <p align="center"><font size="3"><b>SYSTEMATIC PALEONTOLOGY</b></font></p>      ]]></body>
<body><![CDATA[<p align="justify">Order <u>Terebratulida</u> WAAGEN, 1883    <br> Suborder Terebratulidina WAAGEN, 1883    <br> Superfamily Terebratuloidea GRAY, 1840    <br> Family Sellithyrididae MUIR-WOOD, 1965    <br> Subfamily Sellithyridinae MUIR-WOOD, 1965    <br> Genus Sellithyris MIDDLEMISS, 1959</p>      <p align="justify">Sellithyris sella (J. de C. Sowerby, 1823)  (<a href="img/revistas/boge/v31n2/v31n2a10f2.jpg" target="_blank">FIGURE 2</a>)</p>      <p align="justify">Description: Pentagonal shell, smooth, maximum wide slightly anterior mid line, anterior commissure episulcate, median sinus smaller and narrower than the lateral, umbo sub-erect. Loop wide and triangular with high-arched transverse band. Other internal features are not observed. Dimensions in the <a href="img/revistas/boge/v31n2/v31n2a10t1.jpg" target="_blank">TABLE 1</a>.    <br> Material examined: Two complete specimen and six internal molds.</p>      <p align="center"><img src="img/revistas/boge/v31n2/v31n2a10f3.jpg"></p>      ]]></body>
<body><![CDATA[<p align="center"><font size="3"><b>IMPLICATIONS</b></font></p>      <p align="justify">The occurrence of <i>Sellithyris sella</i> in the Rosablanca Formation from Zapatoca, Santander Province, and Santa Sofia, Boyac&aacute; province suggest that it was widely distributed during Late Valanginian&ndash;?Hauterivian in Colombia and confirms the direct transatlantic connections with Western Europe.    <br> Recently, Gaspard (2005) observed shape variations in <i>Sellithysis cenomanensis</i> from Sarthe, Charente-maritime, Indre et Loire, Maine et Loire, Vend&eacute;e and S.E. France, associated to the position during the Cenomanian boreal and mesogean provinces. Gaspard (2005) suggested that the brachiopods react quickly to the environmental modification to explain the observed variations. Then, the extensive morphological study of <i>Sellithyris</i> could to improve the understanding of the relationship between Andean and Tethyan realms.</p>  <hr>      <p align="center"><font size="3"><b>REFERENCIAS</b></font></p>      <!-- ref --><p align="justify">Dietrich, W. 1938. Lamelibranquios cret&aacute;cicos de la Cordillera Oriental. En. Scheibe, R.: <i>Estudios geol&oacute;gicos y paleontol&oacute;gicos sobre la Cordillera Oriental de Colombia</i>. Minist. Ind. y Petrol,. (2), 7-80 Parte tercera, pp. 81-108, pl. 2. Bogot&aacute;.&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=000037&pid=S0120-0283200900020001000001&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --><!-- ref --><p align="justify">Gaspard, D. 2005. Shape variation in Cretaceous biplicate terebratulid brachiopods. 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