FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4221075818> ?p ?o ?g. }

• W4221075818 abstract "<strong class=journal-contentHeaderColor>Abstract.</strong> This paper provides a summary of published sea-level archives representing the past position of sea level during the Last Interglacial sea-level highstand in the Bahamas, Turks and Caicos, and the eastern (Atlantic) coast of Florida, USA. These data were assembled as part of a community effort to build the World Atlas of Last Interglacial Shorelines (WALIS) database. Shallow marine deposits from this sea-level highstand are widespread across the region and are dominated by carbonate sedimentary features. In addition to depositional (constructional) sedimentary indicators of past sea-level position, there is also evidence of erosion, dissolution, and/or subaerial exposure in places that can place an upper limit on the position of sea level. The sea-level indicators that have been observed within this region and attributed to Marine Isotope Stage (MIS) 5e include corals, oolites, and other coastal sedimentary features. Here we compile a total of 50 relative sea-level indicators including 36 in the Bahamas, three in West Caicos, and a remaining 10 for the eastern seaboard of Florida. We have also compiled U-Th age data for 24 fossil corals and 56 oolite samples. While some of these archives have been dated using U-Th disequilibrium methods, amino acid racemization, or optically stimulated luminescence, other features have more uncertain ages that have been deduced in the context of regional mapping and stratigraphy. Sedimentary archives in this region that constrain the elevation of the past position of sea level are associated with uncertainties that range from a couple of decimeters to several meters. Across the Bahamas and on West Caicos, one of the observations that emerges from this compilation is that estimation of sea-level position in this region during Marine Isotope Stage 5e is complicated by widespread stratigraphic evidence for at least one sea-level oscillation. This evidence is defined by submarine features separated by erosion and subaerial exposure, meaning that there were likely multiple distinct peaks in sea level rather than just one. To this end, the timing of these individual sea-level indicators becomes important when compiling and comparing data across the region given that different archives may have formed during different sub-orbital peaks in sea level. The database can be found at <a href=https://doi.org/10.5281/zenodo.5596898>https://doi.org/10.5281/zenodo.5596898</a> (Dutton et al., 2021)." @default.
• W4221075818 created "2022-04-03" @default.
• W4221075818 creator A5086608588 @default.
• W4221075818 date "2022-03-17" @default.
• W4221075818 modified "2023-09-30" @default.
• W4221075818 title "Reply on RC2" @default.
• W4221075818 doi "https://doi.org/10.5194/essd-2021-391-ac2" @default.
• W4221075818 hasPublicationYear "2022" @default.
• W4221075818 type Work @default.
• W4221075818 citedByCount "0" @default.
• W4221075818 crossrefType "peer-review" @default.
• W4221075818 hasAuthorship W4221075818A5086608588 @default.
• W4221075818 hasBestOaLocation W42210758181 @default.
• W4221075818 hasConcept C109007969 @default.
• W4221075818 hasConcept C111368507 @default.
• W4221075818 hasConcept C126753816 @default.
• W4221075818 hasConcept C127313418 @default.
• W4221075818 hasConcept C151730666 @default.
• W4221075818 hasConcept C15739521 @default.
• W4221075818 hasConcept C186240526 @default.
• W4221075818 hasConcept C2780518792 @default.
• W4221075818 hasConcept C6494504 @default.
• W4221075818 hasConcept C74501621 @default.
• W4221075818 hasConcept C84983702 @default.
• W4221075818 hasConceptScore W4221075818C109007969 @default.
• W4221075818 hasConceptScore W4221075818C111368507 @default.
• W4221075818 hasConceptScore W4221075818C126753816 @default.
• W4221075818 hasConceptScore W4221075818C127313418 @default.
• W4221075818 hasConceptScore W4221075818C151730666 @default.
• W4221075818 hasConceptScore W4221075818C15739521 @default.
• W4221075818 hasConceptScore W4221075818C186240526 @default.
• W4221075818 hasConceptScore W4221075818C2780518792 @default.
• W4221075818 hasConceptScore W4221075818C6494504 @default.
• W4221075818 hasConceptScore W4221075818C74501621 @default.
• W4221075818 hasConceptScore W4221075818C84983702 @default.
• W4221075818 hasLocation W42210758181 @default.
• W4221075818 hasOpenAccess W4221075818 @default.
• W4221075818 hasPrimaryLocation W42210758181 @default.
• W4221075818 hasRelatedWork W1974627273 @default.
• W4221075818 hasRelatedWork W2036298535 @default.
• W4221075818 hasRelatedWork W205666370 @default.
• W4221075818 hasRelatedWork W2077400710 @default.
• W4221075818 hasRelatedWork W2089564150 @default.
• W4221075818 hasRelatedWork W2485140744 @default.
• W4221075818 hasRelatedWork W281964413 @default.
• W4221075818 hasRelatedWork W3161412770 @default.
• W4221075818 hasRelatedWork W4320487448 @default.
• W4221075818 hasRelatedWork W943716509 @default.
• W4221075818 isParatext "false" @default.
• W4221075818 isRetracted "false" @default.
• W4221075818 workType "peer-review" @default.