Item talk:Q239983
From geokb
{
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Pinter et al.\u2019s discussion emphasizes and reinforces some of the important concepts we presented but also raises questions regarding specific aspects of our study, including that: (1) base level is the dominant control on fluvial system change on Santa Rosa Island (SRI); (2) post-Last Glacial Maximum (LGM) fluvial aggradation on SRI occurred at uniform rates; and (3) the transition from aggradation to incision on SRI occurred during the last 500 to \u2264150 years.", "description": "3 p.", "publisher": { "@type": "Organization", "name": "Elsevier" }, "author": [ { "@type": "Person", "name": "Pigati, Jeffrey S. jpigati@usgs.gov", "givenName": "Jeffrey S.", "familyName": "Pigati", "email": "jpigati@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-5843-6219", "url": "https://orcid.org/0000-0001-5843-6219" }, "affiliation": [ { "@type": "Organization", "name": "Geosciences and Environmental Change Science Center", "url": "https://www.usgs.gov/centers/geosciences-and-environmental-change-science-center" } ] }, { "@type": "Person", "name": "Schumann, R. 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