{"id":{"repo_id":"loma-linda","oai_identifier":"oai:scholarsrepository.llu.edu:etd-1706"},"canonical_url":"https://search.dev.ndltd.org/etd/loma-linda/oai:scholarsrepository.llu.edu:etd-1706","repository":{"repo_id":"loma-linda","name":"Loma Linda University","base_url":"https://scholarsrepository.llu.edu/do/oai/"},"display":{"title":"The Relation of Temperature to Calcification in MONTIPORA VERRUCOSA","abstract":"<p>A method for quantitatively comparing calcification rates in coral was used to find an optimum growth temperature for <em>Montipora verrueosa.</em> This method is based on the uptake of the radioactive isotope ca<sup>45</sup>. By supplying the water the corals are growing i·n with a known amount of radioactivity and comparing this with the activity of the coral samples, a rate of Ca<sup>45</sup>C0<sub>3 </sub>incorporation can be determined per unit of time. </p> <p>Various tests show that inorganic exchange does not appear to be a significant factor in interpretation of the results obtained. The edge of a colony calcifies faster than other parts, and the upper surface calcifies faster than the lower. Tests run at various temperatures between 17° C and 34° C indicate that the optimum temperature for calcification is around 30° C.</p>","abstract_html":"&lt;p&gt;A method for quantitatively comparing calcification rates in coral was used to find an optimum growth temperature for &lt;em&gt;Montipora verrueosa.&lt;/em&gt; This method is based on the uptake of the radioactive isotope ca&lt;sup&gt;45&lt;/sup&gt;. By supplying the water the corals are growing i·n with a known amount of radioactivity and comparing this with the activity of the coral samples, a rate of Ca&lt;sup&gt;45&lt;/sup&gt;C0&lt;sub&gt;3 &lt;/sub&gt;incorporation can be determined per unit of time. &lt;/p&gt; &lt;p&gt;Various tests show that inorganic exchange does not appear to be a significant factor in interpretation of the results obtained. The edge of a colony calcifies faster than other parts, and the upper surface calcifies faster than the lower. Tests run at various temperatures between 17° C and 34° C indicate that the optimum temperature for calcification is around 30° C.&lt;/p&gt;","abstract_has_math":false,"creators":["Cox, Walter W."],"institution":null,"degree_name":"Master of Arts (MA)","degree_level":"Thesis","degree_discipline":"Biology","degree_department":null,"school":null,"contributors":["Ariel A. Roth","Leonard R. Brand","Arthur V. Chadwick"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1971,"date_issued":"1971-08-01T07:00:00Z","date_published":"1971-08-01T07:00:00Z","updated_at":"2026-07-24T02:52:59Z","subjects":["Biology","Corals"],"languages":["English"],"rights":["This title appears here courtesy of the author, who has granted Loma Linda University a limited, non-exclusive right to make this publication available to the public. The author retains all other copyrights."],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"https://scholarsrepository.llu.edu/etd/615","outbound_label":"Repository record","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Ariel A. Roth","Leonard R. Brand","Arthur V. Chadwick"]},{"key":"dc:creator","label":"Author","values":["Cox, Walter W."]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"thesis:degree_discipline","label":"Discipline","values":["Biology"]},{"key":"thesis:degree_level","label":"Degree Level","values":["Thesis"]},{"key":"thesis:degree_name","label":"Degree Name","values":["Master of Arts (MA)"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Biology","Corals"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language","label":"Dc Language","values":["English"]},{"key":"dc:rights","label":"Dc Rights","values":["This title appears here courtesy of the author, who has granted Loma Linda University a limited, non-exclusive right to make this publication available to the public. The author retains all other copyrights."]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["https://scholarsrepository.llu.edu/etd/615"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["<p>A method for quantitatively comparing calcification rates in coral was used to find an optimum growth temperature for <em>Montipora verrueosa.</em> This method is based on the uptake of the radioactive isotope ca<sup>45</sup>. By supplying the water the corals are growing i·n with a known amount of radioactivity and comparing this with the activity of the coral samples, a rate of Ca<sup>45</sup>C0<sub>3 </sub>incorporation can be determined per unit of time. </p> <p>Various tests show that inorganic exchange does not appear to be a significant factor in interpretation of the results obtained. The edge of a colony calcifies faster than other parts, and the upper surface calcifies faster than the lower. Tests run at various temperatures between 17° C and 34° C indicate that the optimum temperature for calcification is around 30° C.</p>"]},{"key":"dc:title","label":"Title","values":["The Relation of Temperature to Calcification in MONTIPORA VERRUCOSA"]}]}],"canonical_facts":{"dc:contributor":["Ariel A. Roth","Leonard R. Brand","Arthur V. Chadwick"],"dc:creator":["Cox, Walter W."],"dc:description.abstract":["<p>A method for quantitatively comparing calcification rates in coral was used to find an optimum growth temperature for <em>Montipora verrueosa.</em> This method is based on the uptake of the radioactive isotope ca<sup>45</sup>. By supplying the water the corals are growing i·n with a known amount of radioactivity and comparing this with the activity of the coral samples, a rate of Ca<sup>45</sup>C0<sub>3 </sub>incorporation can be determined per unit of time. </p> <p>Various tests show that inorganic exchange does not appear to be a significant factor in interpretation of the results obtained. The edge of a colony calcifies faster than other parts, and the upper surface calcifies faster than the lower. Tests run at various temperatures between 17° C and 34° C indicate that the optimum temperature for calcification is around 30° C.</p>"],"dc:identifier":["https://scholarsrepository.llu.edu/etd/615"],"dc:language":["English"],"dc:rights":["This title appears here courtesy of the author, who has granted Loma Linda University a limited, non-exclusive right to make this publication available to the public. The author retains all other copyrights."],"dc:subject":["Biology","Corals"],"dc:title":["The Relation of Temperature to Calcification in MONTIPORA VERRUCOSA"],"thesis:degree_discipline":["Biology"],"thesis:degree_level":["Thesis"],"thesis:degree_name":["Master of Arts (MA)"]},"updated_at":"2026-07-24T02:52:59Z"}