FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4367394588> ?p ?o ?g. }

• W4367394588 endingPage "938" @default.
• W4367394588 startingPage "926" @default.
• W4367394588 abstract "The late-Quaternary relative sea-level (RSL) history of Ireland is complex, positioned at the margins of the former British-Irish Ice Sheet, and subject to the influence of ice unloading and forebulge collapse. Geophysical models of post-glacial isostatic adjustment (GIA) provide estimates of the pattern of RSL change since deglaciation which may be tested and validated with empirical data from proxy records. For the region of northwest Ireland, there is a paucity of high-quality RSL data and, therefore, equivocal evidence to support the GIA models that predict a mid to Late-Holocene RSL highstand of between +0.5 and +2 m above present. This study aims to investigate this model-data discrepancy by reconstructing RSL change from a near continuous salt-marsh sequence at Bracky Bridge, Donegal, spanning the last ca. 2500 years. We develop a transfer function model to reconstruct the vertical position of sea level using a regional diatom training set to quantify the indicative meaning and predict the palaeomarsh elevation of the core samples. A chronology is provided by a combination of 14 C and 210 Pb data, with sample specific ages derived from an age-depth model using a Bayesian framework. Our reconstruction shows ca. 2 m of relative sea-level rise in the past 2500 years. This is not compatible with some previously published sea-level index points from the region, which we re-interpret as freshwater/terrestrial limiting data. These results do not provide any evidence to support a Mid-Holocene RSL highstand above present sea level. Whilst none of the available GIA models replicate the timing and magnitude of the Late-Holocene RSL rise in our reconstruction, those which incorporate a thick and extensive British-Irish Sea Ice Sheet provide the best fit." @default.
• W4367394588 created "2023-04-30" @default.
• W4367394588 creator A5001929892 @default.
• W4367394588 creator A5042625756 @default.
• W4367394588 creator A5061349777 @default.
• W4367394588 date "2023-04-29" @default.
• W4367394588 modified "2023-09-26" @default.
• W4367394588 title "Holocene relative sea-level changes in northwest Ireland: An empirical test for glacial isostatic adjustment models" @default.
• W4367394588 cites W140492274 @default.
• W4367394588 cites W1540089290 @default.
• W4367394588 cites W1562504550 @default.
• W4367394588 cites W180535233 @default.
• W4367394588 cites W1882030935 @default.
• W4367394588 cites W1964458179 @default.
• W4367394588 cites W1966852422 @default.
• W4367394588 cites W1983594297 @default.
• W4367394588 cites W1990639855 @default.
• W4367394588 cites W1995403074 @default.
• W4367394588 cites W2002459488 @default.
• W4367394588 cites W2029626186 @default.
• W4367394588 cites W2041157598 @default.
• W4367394588 cites W2042584557 @default.
• W4367394588 cites W2043403145 @default.
• W4367394588 cites W2045573011 @default.
• W4367394588 cites W2047786034 @default.
• W4367394588 cites W2057429163 @default.
• W4367394588 cites W2059516882 @default.
• W4367394588 cites W2076358297 @default.
• W4367394588 cites W2082947006 @default.
• W4367394588 cites W2083680802 @default.
• W4367394588 cites W2084248277 @default.
• W4367394588 cites W2085216145 @default.
• W4367394588 cites W2085545753 @default.
• W4367394588 cites W2098679437 @default.
• W4367394588 cites W2106029620 @default.
• W4367394588 cites W2109862542 @default.
• W4367394588 cites W2111895884 @default.
• W4367394588 cites W2115595032 @default.
• W4367394588 cites W2122364619 @default.
• W4367394588 cites W2138545570 @default.
• W4367394588 cites W2164185981 @default.
• W4367394588 cites W2167941657 @default.
• W4367394588 cites W2173410598 @default.
• W4367394588 cites W2269341987 @default.
• W4367394588 cites W2269637330 @default.
• W4367394588 cites W2293957909 @default.
• W4367394588 cites W2605116112 @default.
• W4367394588 cites W2756742426 @default.
• W4367394588 cites W2797343474 @default.
• W4367394588 cites W2904154839 @default.
• W4367394588 cites W2949809767 @default.
• W4367394588 cites W2963431494 @default.
• W4367394588 cites W3015391807 @default.
• W4367394588 cites W3037900220 @default.
• W4367394588 cites W3083605471 @default.
• W4367394588 cites W3168297185 @default.
• W4367394588 cites W3184346096 @default.
• W4367394588 cites W3210321671 @default.
• W4367394588 cites W4231824221 @default.
• W4367394588 cites W4234179774 @default.
• W4367394588 cites W4244520808 @default.
• W4367394588 cites W4255913764 @default.
• W4367394588 cites W4294904775 @default.
• W4367394588 doi "https://doi.org/10.1177/09596836231169992" @default.
• W4367394588 hasPublicationYear "2023" @default.
• W4367394588 type Work @default.
• W4367394588 citedByCount "0" @default.
• W4367394588 crossrefType "journal-article" @default.
• W4367394588 hasAuthorship W4367394588A5001929892 @default.
• W4367394588 hasAuthorship W4367394588A5042625756 @default.
• W4367394588 hasAuthorship W4367394588A5061349777 @default.
• W4367394588 hasBestOaLocation W43673945881 @default.
• W4367394588 hasConcept C100970517 @default.
• W4367394588 hasConcept C111368507 @default.
• W4367394588 hasConcept C123750103 @default.
• W4367394588 hasConcept C127313418 @default.
• W4367394588 hasConcept C140345934 @default.
• W4367394588 hasConcept C140711978 @default.
• W4367394588 hasConcept C151730666 @default.
• W4367394588 hasConcept C15739521 @default.
• W4367394588 hasConcept C180705331 @default.
• W4367394588 hasConcept C205649164 @default.
• W4367394588 hasConcept C49204034 @default.
• W4367394588 hasConcept C74501621 @default.
• W4367394588 hasConceptScore W4367394588C100970517 @default.
• W4367394588 hasConceptScore W4367394588C111368507 @default.
• W4367394588 hasConceptScore W4367394588C123750103 @default.
• W4367394588 hasConceptScore W4367394588C127313418 @default.
• W4367394588 hasConceptScore W4367394588C140345934 @default.
• W4367394588 hasConceptScore W4367394588C140711978 @default.
• W4367394588 hasConceptScore W4367394588C151730666 @default.
• W4367394588 hasConceptScore W4367394588C15739521 @default.
• W4367394588 hasConceptScore W4367394588C180705331 @default.
• W4367394588 hasConceptScore W4367394588C205649164 @default.
• W4367394588 hasConceptScore W4367394588C49204034 @default.
• W4367394588 hasConceptScore W4367394588C74501621 @default.
• W4367394588 hasIssue "8" @default.
• W4367394588 hasLocation W43673945881 @default.

• next