FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2896422742> ?p ?o ?g. }

• W2896422742 endingPage "146" @default.
• W2896422742 startingPage "124" @default.
• W2896422742 abstract "We have assembled a database of Relative Sea Level (RSL) data points from the eastern coast of Canada from Hudson Bay to the border with the USA. In compiling this database we have critically reviewed 1092 radiocarbon dated samples from raised beaches, isolation basins, intertidal and marine deposits, and archaeological indicators to produce 405 sea-level index points and 687 sea-level limiting points. Our comprehensive, systematic, and quality-controlled RSL database allowed for the reconstruction of the postglacial evolution of 34 regions of eastern Canada providing new basin-scale insights into the processes driving RSL changes in the last ∼16 ka. The combination of a database of sea-level index points with an innovative empirical-Bayesian spatio-temporal statistical model provided new insights into rates and magnitude of the spatially-variable glacial isostatic adjustment (GIA), which dominated the postglacial RSL evolution in this sector of North America. A continuous postglacial RSL fall is observed at latitudes ≥ ∼50° N with higher rates (up to 35 mm a−1) recorded in southeastern Hudson Bay. At lower latitudes, the evolution is non-monotonic with RSL that dropped to a spatially variable early-Holocene lowstand, followed by a mid-Holocene highstand and, eventually, a gradual drop to present RSL. This pattern is particularly evident in the St Lawrence corridor. Along the majority of the Newfoundland, New Brunswick and western Nova Scotia coasts, a late-Pleistocene/early-Holocene RSL lowstand was followed by a continuous rise through the Holocene. At the margin of the former ice-sheet (i.e. eastern Nova Scotia), our data identify a continuous RSL rise through the Holocene. These records are characterized by decreasing rates of RSL rise through time, commencing with a rapid rise during the early Holocene (up to ∼17 mm a−1), a slowdown in the mid-Holocene (average rates ≤ ∼9 mm a−1), and a further reduction in the late Holocene (average rates < 2 mm a−1). Finally, our database allowed the identification of regions, including the Labrador coast and part of the St Lawrence corridor, where further investigations are required to better constrain the RSL evolution and improve our ability to assess the variability of RSL histories." @default.
• W2896422742 created "2018-10-26" @default.
• W2896422742 creator A5004126647 @default.
• W2896422742 creator A5024136135 @default.
• W2896422742 creator A5024860521 @default.
• W2896422742 creator A5040508364 @default.
• W2896422742 creator A5061718318 @default.
• W2896422742 creator A5078851706 @default.
• W2896422742 creator A5080313267 @default.
• W2896422742 creator A5084053928 @default.
• W2896422742 date "2018-12-01" @default.
• W2896422742 modified "2023-10-17" @default.
• W2896422742 title "Postglacial relative sea-level histories along the eastern Canadian coastline" @default.
• W2896422742 cites W1494499287 @default.
• W2896422742 cites W1515483066 @default.
• W2896422742 cites W1525255738 @default.
• W2896422742 cites W1540946605 @default.
• W2896422742 cites W1562504550 @default.
• W2896422742 cites W1563982272 @default.
• W2896422742 cites W1564214155 @default.
• W2896422742 cites W1581658614 @default.
• W2896422742 cites W1597233176 @default.
• W2896422742 cites W1605744938 @default.
• W2896422742 cites W1646758270 @default.
• W2896422742 cites W1733916393 @default.
• W2896422742 cites W1742879260 @default.
• W2896422742 cites W1859646104 @default.
• W2896422742 cites W1866401552 @default.
• W2896422742 cites W1875334564 @default.
• W2896422742 cites W1911328977 @default.
• W2896422742 cites W1924853677 @default.
• W2896422742 cites W1947783415 @default.
• W2896422742 cites W1965967607 @default.
• W2896422742 cites W1966429477 @default.
• W2896422742 cites W1970171789 @default.
• W2896422742 cites W1971398007 @default.
• W2896422742 cites W1974798332 @default.
• W2896422742 cites W1977248823 @default.
• W2896422742 cites W1978750157 @default.
• W2896422742 cites W1979155994 @default.
• W2896422742 cites W1980230307 @default.
• W2896422742 cites W1980291384 @default.
• W2896422742 cites W1983672286 @default.
• W2896422742 cites W1987613981 @default.
• W2896422742 cites W1988155239 @default.
• W2896422742 cites W1989459572 @default.
• W2896422742 cites W1989956469 @default.
• W2896422742 cites W1990028434 @default.
• W2896422742 cites W1990477265 @default.
• W2896422742 cites W1993187434 @default.
• W2896422742 cites W1995390085 @default.
• W2896422742 cites W1997930801 @default.
• W2896422742 cites W1998764664 @default.
• W2896422742 cites W2008724523 @default.
• W2896422742 cites W2009721490 @default.
• W2896422742 cites W2013828431 @default.
• W2896422742 cites W2015211281 @default.
• W2896422742 cites W2017717160 @default.
• W2896422742 cites W2024211871 @default.
• W2896422742 cites W2024369723 @default.
• W2896422742 cites W2027001806 @default.
• W2896422742 cites W2027850209 @default.
• W2896422742 cites W2031669613 @default.
• W2896422742 cites W2032923880 @default.
• W2896422742 cites W2032939543 @default.
• W2896422742 cites W2034239681 @default.
• W2896422742 cites W2034538472 @default.
• W2896422742 cites W2036107840 @default.
• W2896422742 cites W2036536434 @default.
• W2896422742 cites W2037884869 @default.
• W2896422742 cites W2038532360 @default.
• W2896422742 cites W2039963712 @default.
• W2896422742 cites W2042554483 @default.
• W2896422742 cites W2043975674 @default.
• W2896422742 cites W2044293086 @default.
• W2896422742 cites W2045088484 @default.
• W2896422742 cites W2046936370 @default.
• W2896422742 cites W2047400748 @default.
• W2896422742 cites W2053864207 @default.
• W2896422742 cites W2054134817 @default.
• W2896422742 cites W2055866586 @default.
• W2896422742 cites W2056144208 @default.
• W2896422742 cites W2057774176 @default.
• W2896422742 cites W2058968253 @default.
• W2896422742 cites W2059472387 @default.
• W2896422742 cites W2062237254 @default.
• W2896422742 cites W2067146014 @default.
• W2896422742 cites W2067750013 @default.
• W2896422742 cites W2070370342 @default.
• W2896422742 cites W2070549462 @default.
• W2896422742 cites W2073290345 @default.
• W2896422742 cites W2074812620 @default.
• W2896422742 cites W2084248277 @default.
• W2896422742 cites W2088640598 @default.
• W2896422742 cites W2091435652 @default.
• W2896422742 cites W2094033454 @default.
• W2896422742 cites W2094350389 @default.
• W2896422742 cites W2094666610 @default.

• next