<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/"
xmlns:dc="http://purl.org/dc/elements/1.1/">
  <dc:title>North American cyclocrinitid algae /</dc:title>
  <dc:creator>Nitecki, Matthew H.</dc:creator>
  <dc:type>text</dc:type>
  <dc:publisher>[Chicago] Field Museum of Natural
History,</dc:publisher>
  <dc:date>1970.</dc:date>
  <dc:language>eng</dc:language>
  <dc:description>p. vii-[xiv], 182 p. 24 cm.</dc:description>
  <dc:description>Cyclocrinitids are marine dasycladaceous algae of
Ordovician and Silurian age. Their skeletal elements consist of a seldom
calcified main axis on which lateral branches are borne in whorls.
Calcified heads commonly form at the termini of the laterals. In North
America cyclocrinitids are represented by three genera: Anomaloides,
Cyclocrinites, and Lepidolites. Anomaloides (=Anomalospongia) possesses
laterals calcified throughout their extent. They expand gently outward, and
no heads form. Three secondary laterals form threadlike projections at the
terminus of each lateral. -- Cyclocrinites (=Cyclocrinus, Lunulites,
Cerionites, Pasceolus, Mastopora, and Nidulites) with a globose thallus is
the most diversified genus. The laterals expand at the termini and form
generally six-sided heads. In one species the laterals branch to the second
degree. The lateral heads are in some species supported by four to six
ribs. In at least one species the laterals constrict twice and form two
layers of heads, one above the other. The main axis is generally short, and
attachment is by means of a pedicle that is, however, frequently not
preserved. Calcification generally occurs above and below the lateral
heads. One new species, Cyclocrinites welleri, is described. -- Lepidolites
consists of one species only and is the most modified of all
cyclocrinitids. The laterals are short, small, and calcified; their ends
are modified and form overlapping plates. -- The cyclocrinitids have been
variously assigned by many authors to many groups, particularly as an
appendix to the sponges. They are here considered a basal receptaculitid
stock that possesses the simplest structures. They fill an important gap in
the fossil record of Paleozoic algae.</dc:description>
  <dc:description>"November 16, 1970."</dc:description>
  <dc:description>Includes bibliographical references (p.
165-182).</dc:description>
  <dc:description>Pt. I: Introduction -- Previous major publications
-- Morphology -- Taxonomic position -- Ecology -- Pt. II: Systematic
descriptions -- Pt. III: Original definitions and descriptions of other
authors. -- Annotated bibliography.</dc:description>
  <dc:description>Fieldiana series has been published as Geological
Series by Field Columbian Museum (1895-1909) and Field Museum of Natural
History (1909-1943), and as Fieldiana: Geology by Chicago Natural History
Museum (1945-1966) and Field Museum of Natural History
(1966-).</dc:description>
  <dc:subject>Dasycladaceae, Fossil.</dc:subject>
  <dc:subject>Paleontology -- Silurian.</dc:subject>
  <dc:subject>Paleontology -- Ordovician.</dc:subject>
  <dc:subject>Paleontology -- North America.</dc:subject>
</oai_dc:dc>
