93 lines
9.7 KiB
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93 lines
9.7 KiB
XML
<document id="DBC2CFEE00F99BD2FB7A3DD56E93B8EA" ID-DOI="10.26879/678" ID-ISSN="1094-8074" ID-Zenodo-Dep="13344530" ID-ZooBank="A085E4EE-97FA-4BB7-AE08-C1674AADAF40" IM.bibliography_requiresApprovalFor="GgImagineBatch" IM.illustrations_approvedBy="carolina" IM.materialsCitations_approvedBy="felipe" IM.metadata_approvedBy="carolina" IM.tables_approvedBy="carolina" IM.taxonomicNames_approvedBy="carolina" IM.treatments_approvedBy="carolina" checkinTime="1723486021566" checkinUser="felipe" docAuthor="Freudenthal, Matthijs & Martín-Suárez, Elvira" docDate="2017" docId="03A2BA4EDF48FF88FF64D911FADF415B" docLanguage="en" docName="PalaeontolElectron.20.2.41A.pdf" docOrigin="Palaeontologia Electronica 9 (1)" docSource="http://dx.doi.org/10.26879/678" docStyle="DocumentStyle:D7620D4238C1CBB81D040B36F8D88A9A.1:PalaeontolElectron.2012-2017.journal_article" docStyleId="D7620D4238C1CBB81D040B36F8D88A9A" docStyleName="PalaeontolElectron.2012-2017.journal_article" docStyleVersion="1" docTitle="A revision of European Plesiosminthus (Rodentia, Dipodidae), and new material from the upper Oligocene of Teruel (Spain)" docType="treatment" docVersion="2" lastPageNumber="3" masterDocId="FF9BC236DF4AFF8AFFA4DD3FFFF44757" masterDocTitle="A revision of European Plesiosminthus (Rodentia, Dipodidae), and new material from the upper Oligocene of Teruel (Spain)" masterLastPageNumber="25" masterPageNumber="1" pageNumber="3" updateTime="1724088668207" updateUser="ExternalLinkService" zenodo-license-document="CC-BY-NC-SA-4.0">
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<mods:title id="1924B6747A2380DB49D2D56F605BF401">A revision of European Plesiosminthus (Rodentia, Dipodidae), and new material from the upper Oligocene of Teruel (Spain)</mods:title>
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<mods:namePart id="FE7E0FF76420514B63A8B08BAE501D52">Freudenthal, Matthijs</mods:namePart>
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<mods:namePart id="9FFF5E6CA7DB3D810D1189AAA5A15D9D">Martín-Suárez, Elvira</mods:namePart>
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<mods:title id="E0AF8F4F34B9EA8BF9D1C430BBFA611D">Palaeontologia Electronica</mods:title>
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<mods:date id="DCCF58CFA2D6DA548C4912A67EF7ACB3">2017</mods:date>
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<mods:number id="C818A538BA351F9B5993FF8ED3ACE096">2017-08-31</mods:number>
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<treatment id="03A2BA4EDF48FF88FF64D911FADF415B" ID-DOI="http://doi.org/10.5281/zenodo.13344536" ID-Zenodo-Dep="13344536" LSID="urn:lsid:plazi:treatment:03A2BA4EDF48FF88FF64D911FADF415B" httpUri="http://treatment.plazi.org/id/03A2BA4EDF48FF88FF64D911FADF415B" lastPageNumber="3" pageId="2" pageNumber="3">
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<subSubSection id="C31158D3DF48FF88FF64D911FADF415B" pageId="2" pageNumber="3" type="description">
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<paragraph id="8BB40B58DF48FF88FF64D911FD524330" blockId="2.[192,793,1070,1799]" pageId="2" pageNumber="3">the anteroloph in M1; antecingulum, a cingulum ridge at the base of the anteroloph in M1.</paragraph>
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<paragraph id="8BB40B58DF48FF88FF5ED951FE804390" blockId="2.[192,793,1070,1799]" pageId="2" pageNumber="3">
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V' is the coefficient of variation (Range divided by median) as defined by
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<bibRefCitation id="EF9A76A9DF48FF88FE56D9B1FE844390" author="Freudenthal, M. & Cuenca Bescos, G." pageId="2" pageNumber="3" pagination="1 - 28" refId="ref13835" refString="Freudenthal, M. and Cuenca Bescos, G. 1984. Size variation of fossil rodent populations. Scripta Geologica, 76: 1 - 28." type="journal article" year="1984">Freudenthal and Cuenca Bescós (1984)</bibRefCitation>
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.
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</paragraph>
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<paragraph id="8BB40B58DF48FF88FF5ED9F1FEC4421F" blockId="2.[192,793,1070,1799]" pageId="2" pageNumber="3">
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Photographs were taken on the electron microscope FEI ESEM QUANTA 400 of the ‘Centro de Instrumentación Científica’ of the University of
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<collectingCountry id="F31C4BC8DF48FF88FF64D811FED8421F" box="[192,300,1326,1352]" name="Grenada" pageId="2" pageNumber="3">Granada</collectingCountry>
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.
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</paragraph>
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<paragraph id="8BB40B58DF48FF88FF5ED871FDC94170" blockId="2.[192,793,1070,1799]" pageId="2" pageNumber="3">Measurements were taken with a Wild M8 binocular microscope, equipped with a mechanical stage with electronic sensors, connected to a computer through a Sony Magnescale measuring unit. The measurement data were processed using a private computer program, written in Visual Basic. Measurements are given in mm.</paragraph>
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<paragraph id="8BB40B58DF48FF88FF5EDB11FEEC41F0" blockId="2.[192,793,1070,1799]" pageId="2" pageNumber="3">
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Locality codes are explained in
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<tableCitation id="C6893EE3DF48FF88FDD4DB11FD3D4110" box="[624,713,1582,1607]" captionStart="TABLE 2" captionStartId="3.[190,268,164,187]" captionTargetPageId="3" captionText="TABLE 2. Locality codes, species contents and most important reference of the localities studied. Zones are European mammal zones (Biochrom’97, 1997)." httpUri="http://table.plazi.org/id/DF745BD0DF49FF89FF1ADD9BFDB3478B" pageId="2" pageNumber="3" tableUuid="DF745BD0DF49FF89FF1ADD9BFDB3478B">Table 2</tableCitation>
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. Other abbreviations are: pcdha = protoconid hind arm; m1, m2, m3 = lower molars; M1, M2, M3 = upper molars.
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</paragraph>
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<paragraph id="8BB40B58DF48FF88FF5EDB91FE6E4050" blockId="2.[192,793,1070,1799]" pageId="2" pageNumber="3">
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For some characters morphology values (MV) have been calculated (see
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<bibRefCitation id="EF9A76A9DF48FF88FD82DBF1FCFB41B0" author="Freudenthal, M." box="[550,783,1742,1767]" pageId="2" pageNumber="3" pagination="97 - 173" refId="ref13794" refString="Freudenthal, M. 2004. Gliridae (Rodentia, Mammalia) from the Eocene and Oligocene of the Sierra Palomera (Teruel, Spain). Treballs del Museu de Geologia de Barcelona, 12: 97 - 173." type="journal article" year="2004">Freudenthal, 2004</bibRefCitation>
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), using the equation
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</paragraph>
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<paragraph id="8BB40B58DF48FF88FEF8DA26FD884065" blockId="2.[348,636,1817,1848]" box="[348,636,1817,1848]" pageId="2" pageNumber="3">
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MV = Σ(n-1)
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<subScript id="178F091DDF48FF88FE4EDA26FE0B406F" attach="left" box="[490,511,1817,1848]" fontSize="8" pageId="2" pageNumber="3">fn</subScript>
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/ (C-1)
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<subScript id="178F091DDF48FF88FDE8DA26FD81406F" attach="left" box="[588,629,1817,1848]" fontSize="8" pageId="2" pageNumber="3">Σfn</subScript>
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,
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</paragraph>
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<paragraph id="8BB40B58DF48FF88FCECD911FADF415B" blockId="2.[840,1441,1070,1554]" pageId="2" pageNumber="3">
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where C is the number of character states, and
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<subScript id="178F091DDF48FF88FAD7D911FA72431A" attach="left" box="[1395,1414,1070,1101]" fontSize="8" pageId="2" pageNumber="3">fn</subScript>
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is the observed frequency for the nth character state. For example, if four character states are distinguished, the consecutive states score 0,
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<geoCoordinate id="EE3F6D9FDF48FF88FAF2D9ACFA6943FB" box="[1366,1437,1171,1196]" degrees="0.333" direction="north" orientation="latitude" pageId="2" pageNumber="3" precision="55" value="0.333">0.333</geoCoordinate>
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,
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<geoCoordinate id="EE3F6D9FDF48FF88FCECD98CFC7F439B" box="[840,907,1203,1228]" degrees="0.666" direction="east" orientation="longitude" pageId="2" pageNumber="3" precision="55" value="0.666">0.666</geoCoordinate>
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, and 1.0, respectively. The scores of all specimens are summed up, and the result is divided by the total number of specimens, leading to a value between 0 and 1. MV is typically useful for features, that in fact have a continuous size representation, e.g., for a length: absent/short /medium/ long, and is an approximation of actually measuring the parameter in each specimen, and calculating the mean of the measurements. It may be calculated on actual numbers of specimens, or on percentages; in the latter case
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<subScript id="178F091DDF48FF88FB10D8CCFB2C4145" attach="left" box="[1204,1240,1523,1554]" fontSize="8" pageId="2" pageNumber="3">Σfn</subScript>
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= 100.
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</paragraph>
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</subSubSection>
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</treatment>
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</document> |