<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">388017279</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180307124914.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">161130e199803  xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1017/S0022336000036313</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">S0022336000036313</subfield>
   <subfield code="2">pii</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)cambridge-10.1017/S0022336000036313</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Color patterns in Mississippian (Chesterian) blastoids</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Harold H. Beaver, Alexander J. Fabian]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">Ninety-one specimens of Pentremites Say from the Mississippian Chesterian display color patterns. The darker color patterns represent a thin veneer of pigmented calcite which is barely visible on a polished surface or thin section, but which can be removed with dilute hydrochloric acid. Preservation appears to be best in specimens from shallow marine clays and shales. The patterns represent four color patterns, each consisting of different shades of calcite, and ranging in color from tan to black. Color patterns generally, but not always, cross growth lines. Type 1 has arched chevron patterns on the deltoids, horizontal lines on the radials, and triangular bands on the basals. Type 2 has darkened deltoids or concave chevrons on the deltoids and darkened areas concentric to the radials, and sometimes alternating light and dark bands conforming to growth lines on the radials. Type 3 has sloping lines crossing the radials, concave chevrons on the deltoids, and darkened areas on the lower radials, concentric to the ambulacra and on the basals. Type 4 has dark dots concentric to the lower ambulacra, arched chevrons on the deltoids and transverse lines abutting the radials and on the basals. The color patterns are original and may have been exposed on the outside of the integument.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Copyright © The Paleontological Society</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Beaver</subfield>
   <subfield code="D">Harold H.</subfield>
   <subfield code="u">Department of Geology, Baylor University, Waco, Texas 76798</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Fabian</subfield>
   <subfield code="D">Alexander J.</subfield>
   <subfield code="u">7016 Jackman Rd., Temperance, Michigan 48182</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Journal of Paleontology</subfield>
   <subfield code="d">Cambridge University Press</subfield>
   <subfield code="g">72/2(1998-03), 332-338</subfield>
   <subfield code="x">0022-3360</subfield>
   <subfield code="q">72:2&lt;332</subfield>
   <subfield code="1">1998</subfield>
   <subfield code="2">72</subfield>
   <subfield code="o">JPA</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1017/S0022336000036313</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="908" ind1=" " ind2=" ">
   <subfield code="D">1</subfield>
   <subfield code="a">research-article</subfield>
   <subfield code="2">jats</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">856</subfield>
   <subfield code="E">40</subfield>
   <subfield code="u">https://doi.org/10.1017/S0022336000036313</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Beaver</subfield>
   <subfield code="D">Harold H.</subfield>
   <subfield code="u">Department of Geology, Baylor University, Waco, Texas 76798</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Fabian</subfield>
   <subfield code="D">Alexander J.</subfield>
   <subfield code="u">7016 Jackman Rd., Temperance, Michigan 48182</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">773</subfield>
   <subfield code="E">0-</subfield>
   <subfield code="t">Journal of Paleontology</subfield>
   <subfield code="d">Cambridge University Press</subfield>
   <subfield code="g">72/2(1998-03), 332-338</subfield>
   <subfield code="x">0022-3360</subfield>
   <subfield code="q">72:2&lt;332</subfield>
   <subfield code="1">1998</subfield>
   <subfield code="2">72</subfield>
   <subfield code="o">JPA</subfield>
  </datafield>
  <datafield tag="900" ind1=" " ind2="7">
   <subfield code="b">CC0</subfield>
   <subfield code="u">http://creativecommons.org/publicdomain/zero/1.0</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="898" ind1=" " ind2=" ">
   <subfield code="a">BK010053</subfield>
   <subfield code="b">XK010053</subfield>
   <subfield code="c">XK010000</subfield>
  </datafield>
  <datafield tag="949" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="F">NATIONALLICENCE</subfield>
   <subfield code="b">NL-cambridge</subfield>
  </datafield>
 </record>
</collection>
