FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W19343185> ?p ?o ?g. }

• W19343185 endingPage "108" @default.
• W19343185 startingPage "82" @default.
• W19343185 abstract "Marine invertebrate faunas with mixtures of extralimital southern and extralimital northern faunal elements, called thermally anomalous faunas, have been recognized for more than a century in the Quaternary marine terrace record of the Pacific Coast of North America. Although many mechanisms have been proposed to explain this phenomenon, no single explanation seems to be applicable to all localities where thermally anomalous faunas have been observed. Here, we describe one such thermally anomalous fossil fauna that was studied on the second emergent marine terrace at Eel Point on San Clemente Island. The Eel Point terrace complex is a composite feature, consisting of a narrow upper bench (terrace 2a) and a broader lower bench (terrace 2b). Terrace 2b, previously dated from ∼128 ka to ∼114 ka, was thought to date solely to marine isotope stage (MIS) 5.5, representing the peak of the last interglacial period. Nevertheless, the fauna contains an extralimital northern species and several northward-ranging species, as well as an extralimital southern species and several southward-ranging species. Similar faunas with thermally anomalous elements have also been reported from San Nicolas Island, Point Loma (San Diego County), and Cayucos (San Luis Obispo County), California. U-series dating of corals at those localities shows that the thermally anomalous faunas may be the result of mixing of fossils from both the ∼100-ka (cool-water) and the ∼120-ka (warm-water) sea level high stands. Submergence, erosion, and fossil mixing of the ∼120-ka terraces by the ∼100-ka high-sea stand may have been possible due to glacial isostatic adjustment (GIA) effects on North America, which could have resulted in a higher-than-present local sea level stand at ∼100 ka. The terrace elevation spacing on San Clemente Island is very similar to that on San Nicolas Island, and we hypothesize that a similar mixing took place on San Clemente Island. Existing fossil records from older terraces elsewhere in California also show thermally anomalous elements, indicating that the scenario presented here for the last interglacial complex may have applicability to much of the marine Quaternary record for the Pacific Coast." @default.
• W19343185 created "2016-06-24" @default.
• W19343185 creator A5021845373 @default.
• W19343185 creator A5052197075 @default.
• W19343185 creator A5055336005 @default.
• W19343185 date "2014-01-01" @default.
• W19343185 modified "2023-10-16" @default.
• W19343185 title "Interpreting the Paleozoogeography and Sea Level History of Thermally Anomalous Marine Terrace Faunas: A Case Study from the Last Interglacial Complex of San Clemente Island, California" @default.
• W19343185 cites W1540946605 @default.
• W19343185 cites W1655056763 @default.
• W19343185 cites W1793126971 @default.
• W19343185 cites W1868427130 @default.
• W19343185 cites W1964858761 @default.
• W19343185 cites W1964998320 @default.
• W19343185 cites W1970284110 @default.
• W19343185 cites W1981288644 @default.
• W19343185 cites W1987244610 @default.
• W19343185 cites W1992519610 @default.
• W19343185 cites W1994155113 @default.
• W19343185 cites W1994587749 @default.
• W19343185 cites W2008670387 @default.
• W19343185 cites W2029679293 @default.
• W19343185 cites W2031194081 @default.
• W19343185 cites W2039113673 @default.
• W19343185 cites W2054037980 @default.
• W19343185 cites W2057199947 @default.
• W19343185 cites W2061258326 @default.
• W19343185 cites W2066159885 @default.
• W19343185 cites W2068151576 @default.
• W19343185 cites W2070900036 @default.
• W19343185 cites W2074455940 @default.
• W19343185 cites W2079403436 @default.
• W19343185 cites W2092367603 @default.
• W19343185 cites W2094033454 @default.
• W19343185 cites W2094988303 @default.
• W19343185 cites W2098567981 @default.
• W19343185 cites W2118954287 @default.
• W19343185 cites W2119381853 @default.
• W19343185 cites W2119932679 @default.
• W19343185 cites W2121820020 @default.
• W19343185 cites W2127493276 @default.
• W19343185 cites W2131402166 @default.
• W19343185 cites W2141434375 @default.
• W19343185 cites W2146605432 @default.
• W19343185 cites W2150741383 @default.
• W19343185 cites W2151064682 @default.
• W19343185 cites W2151450181 @default.
• W19343185 cites W2151801251 @default.
• W19343185 cites W2167423623 @default.
• W19343185 cites W2167451751 @default.
• W19343185 cites W2329566195 @default.
• W19343185 doi "https://doi.org/10.3398/042.007.0110" @default.
• W19343185 hasPublicationYear "2014" @default.
• W19343185 type Work @default.
• W19343185 sameAs 19343185 @default.
• W19343185 citedByCount "10" @default.
• W19343185 countsByYear W193431852014 @default.
• W19343185 countsByYear W193431852015 @default.
• W19343185 countsByYear W193431852016 @default.
• W19343185 countsByYear W193431852017 @default.
• W19343185 countsByYear W193431852018 @default.
• W19343185 countsByYear W193431852019 @default.
• W19343185 countsByYear W193431852021 @default.
• W19343185 countsByYear W193431852022 @default.
• W19343185 crossrefType "journal-article" @default.
• W19343185 hasAuthorship W19343185A5021845373 @default.
• W19343185 hasAuthorship W19343185A5052197075 @default.
• W19343185 hasAuthorship W19343185A5055336005 @default.
• W19343185 hasBestOaLocation W193431851 @default.
• W19343185 hasConcept C111368507 @default.
• W19343185 hasConcept C125471540 @default.
• W19343185 hasConcept C127313418 @default.
• W19343185 hasConcept C151730666 @default.
• W19343185 hasConcept C160464908 @default.
• W19343185 hasConcept C166957645 @default.
• W19343185 hasConcept C186240526 @default.
• W19343185 hasConcept C18903297 @default.
• W19343185 hasConcept C205649164 @default.
• W19343185 hasConcept C2776638177 @default.
• W19343185 hasConcept C86803240 @default.
• W19343185 hasConceptScore W19343185C111368507 @default.
• W19343185 hasConceptScore W19343185C125471540 @default.
• W19343185 hasConceptScore W19343185C127313418 @default.
• W19343185 hasConceptScore W19343185C151730666 @default.
• W19343185 hasConceptScore W19343185C160464908 @default.
• W19343185 hasConceptScore W19343185C166957645 @default.
• W19343185 hasConceptScore W19343185C186240526 @default.
• W19343185 hasConceptScore W19343185C18903297 @default.
• W19343185 hasConceptScore W19343185C205649164 @default.
• W19343185 hasConceptScore W19343185C2776638177 @default.
• W19343185 hasConceptScore W19343185C86803240 @default.
• W19343185 hasIssue "1" @default.
• W19343185 hasLocation W193431851 @default.
• W19343185 hasLocation W193431852 @default.
• W19343185 hasOpenAccess W19343185 @default.
• W19343185 hasPrimaryLocation W193431851 @default.
• W19343185 hasRelatedWork W181128007 @default.
• W19343185 hasRelatedWork W1965600959 @default.

• next