<?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>1405-3322</journal-id>
<journal-title><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Soc. Geol. Mex]]></abbrev-journal-title>
<issn>1405-3322</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Geológica Mexicana A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-33222023000300104</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2023v75n3a110923</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[The Hettangian-Bajocian flora of the Shemshak Group, Kerman, Iran]]></article-title>
<article-title xml:lang="es"><![CDATA[La flora Hettangiano-Bajociano del Grupo Shemshak, Kerman, Iran]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ameri]]></surname>
<given-names><![CDATA[Hamed]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Shaghayeghi]]></surname>
<given-names><![CDATA[Parisa]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,University of Advanced Technology  ]]></institution>
<addr-line><![CDATA[Kerman ]]></addr-line>
<country>Islamic Republic of Iran</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Kerman Institute of Higher Education Department of Geology ]]></institution>
<addr-line><![CDATA[Kerman ]]></addr-line>
<country>Islamic Republic of Iran</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<volume>75</volume>
<numero>3</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222023000300104&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222023000300104&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222023000300104&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Numerous examples of macro plant fossils can be found in the Kerman region&#8217;s Early and Middle Jurassic successions. The Ab-e-Haji, Badamu, and Hojedk formations were among these patterns. One of the suitable regions for paleobotanical study is the Chatroud section. In this region, the Lower-Middle Jurassic is approximately 210 meters thick. 18 species of macro plant fossils from 14 genera, including Nilssonia polymorpha, Ptero phyllum nathorsti, Podozamites distans, Elatocladus zamioides, Elatides thomasii, Nilssonia feriziensis, Nilssonia herriesi, and Beania sp., which are identified and described in this study, along with Pterophyllum schenki, Anomozamites marginatus, and Klukia exilis. In this region, there are two plant assemblage zones known as Anomozamites marginatus-Pterophyllum schenki Zone and Klukia exilis Zone. The Hettangian-Bajocian age is preserved at the Chatroud section.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Numerosos ejemplos de macro plantas fósiles pueden ser encontrados en las sucesiones del Jurásico Temprano y Medio de la región de Kerman. Las formaciones Ab-e-Haji, Badamu, y Hojedk se encuentran entre estos patrones. Una de las regiones adecuadas para estudios paleobotánicos es el sección Chatroud. En esta región, el Jurásico Inferior-Medio tine aproximadamente 210 metros de espesor. 18 especies de macrofósiles de plantas de 14 géneros, incluyen Nilssonia polymorpha, Pterophyllum nathorsti, Podozamites distans, Elatocladus zamioides, Elatides thomasii, Nilssonia feriziensis, Nilssonia herriesi y Beania sp., los cuales son identificados y descritos en este estudio, además de Pterophyllum schenki, Anomozamites marginatus y Klukia exilis. En esta región existen dos zonas de asociación de plantas, conocidas como: Zona Anomozamites marginatus-Pterophyllum schenki y Zona Klukia exilis. La edad Hettangian-Bajocian está preservada en la sección Chatroud.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Jurassic]]></kwd>
<kwd lng="en"><![CDATA[Hettangian-Bajocian]]></kwd>
<kwd lng="en"><![CDATA[plants]]></kwd>
<kwd lng="en"><![CDATA[Biozone]]></kwd>
<kwd lng="en"><![CDATA[Kerman]]></kwd>
<kwd lng="en"><![CDATA[Iran]]></kwd>
<kwd lng="es"><![CDATA[Jurásico]]></kwd>
<kwd lng="es"><![CDATA[Hettangiano-Bajociano]]></kwd>
<kwd lng="es"><![CDATA[plan tas]]></kwd>
<kwd lng="es"><![CDATA[Biozona]]></kwd>
<kwd lng="es"><![CDATA[Kerman]]></kwd>
<kwd lng="es"><![CDATA[Irán]]></kwd>
</kwd-group>
</article-meta>
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