Item talk:Q240147
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Extended late Holocene relative sea-level histories for North Carolina, USA", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70193066", "url": "https://pubs.usgs.gov/publication/70193066" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70193066 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1016/j.quascirev.2017.01.012", "url": "https://doi.org/10.1016/j.quascirev.2017.01.012" } ], "journal": { "@type": "Periodical", "name": "Quaternary Science Reviews", "volumeNumber": "160", "issueNumber": null }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Quaternary Science Reviews" } ], "datePublished": "2017", "dateModified": "2017-11-12", "abstract": "We produced \u223c3000-year long relative sea-level (RSL) histories for two sites in North Carolina (USA) using foraminifera preserved in new and existing cores of dated salt-marsh sediment. At Cedar Island, RSL rose by \u223c2.4\u00a0m during the past \u223c3000 years compared to \u223c3.3\u00a0m\u00a0at Roanoke Island. This spatial difference arises primarily from differential GIA that caused late Holocene RSL rise to be 0.1\u20130.2\u00a0mm/yr faster at Roanoke Island than at Cedar Island. However, a non-linear difference in RSL between the two study regions (particularly from \u223c0 CE to \u223c1250 CE) indicates that additional local- to regional-scale processes drove centennial-scale RSL change in North Carolina. Therefore, the Cedar Island and Roanoke Island records should be considered as independent of one another. Between-site differences on sub-millennial timescales cannot be adequately explained by non-stationary tides, sediment compaction, or local sediment dynamics. We propose that a period of accelerating RSL rise from \u223c600 CE to 1100 CE that is present at Roanoke Island (and other sites north of Cape Hatteras at least as far as Connecticut), but absent at Cedar Island (and other sites south of Cape Hatteras at least as far as northeastern Florida) is a local-to regional-scale effect of dynamic ocean and/or atmospheric circulation.", "description": "18 p.", "publisher": { "@type": "Organization", "name": "Elsevier" }, "author": [ { "@type": "Person", "name": "Bernhardt, Christopher E. cbernhardt@usgs.gov", "givenName": "Christopher E.", "familyName": "Bernhardt", "email": "cbernhardt@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0003-0082-4731", "url": "https://orcid.org/0000-0003-0082-4731" }, "affiliation": [ { "@type": "Organization", "name": "Eastern Geology and Paleoclimate Science Center", "url": "https://www.usgs.gov/centers/florence-bascom-geoscience-center" }, { "@type": "Organization", "name": "Florence Bascom Geoscience Center", "url": "https://www.usgs.gov/centers/florence-bascom-geoscience-center" } ] }, { "@type": "Person", "name": "Kemp, Andrew C.", "givenName": "Andrew C.", "familyName": "Kemp", "affiliation": [ { "@type": "Organization", "name": "Tufts University" } ] }, { "@type": "Person", "name": "Kegel, Jessica J.", "givenName": "Jessica J.", "familyName": "Kegel", "affiliation": [ { "@type": "Organization", "name": "East Carolina University Greenville, North Carolina,USA" } ] }, { "@type": "Person", "name": "Culver, Stephen J.", "givenName": "Stephen J.", "familyName": "Culver", "affiliation": [ { "@type": "Organization", "name": "East Carolina University Greenville, North Carolina,USA" } ] }, { "@type": "Person", "name": "Mulligan, Ryan P.", "givenName": "Ryan P.", "familyName": "Mulligan", "affiliation": [ { "@type": "Organization", "name": "Queen's University - Kingston, Ontario" } ] }, { "@type": "Person", "name": "Horton, Benjamin P.", "givenName": 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