Relative sea-level change in Newfoundland, Canada during the past 3000 years
Several processes contributing to coastal relative sea-level (RSL) change in the North Atlantic Ocean are observed and/or predicted to have distinctive spatial expressions that vary by latitude. To expand the latitudinal range of RSL records spanning the past ~3000 years and the likelihood of recogn...
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ftunivmaynooth:oai:mural.maynoothuniversity.ie:13162 2023-05-15T17:21:55+02:00 Relative sea-level change in Newfoundland, Canada during the past 3000 years Kemp, Andrew C. Wright, Alexander J. Edwards, Robin J. Barnett, Robert Brain, Matthew J. Kopp, Robert E. Cahill, Niamh Horton, Benjamin P. Charman, Daniel J. Hawkes, Andrea D. Hill, Troy D. van de Plaasche, Orson 2018 text https://mural.maynoothuniversity.ie/13162/ https://mural.maynoothuniversity.ie/13162/1/NC_maths%26stats_relative.pdf en eng Elsevier https://mural.maynoothuniversity.ie/13162/1/NC_maths%26stats_relative.pdf Kemp, Andrew C. and Wright, Alexander J. and Edwards, Robin J. and Barnett, Robert and Brain, Matthew J. and Kopp, Robert E. and Cahill, Niamh and Horton, Benjamin P. and Charman, Daniel J. and Hawkes, Andrea D. and Hill, Troy D. and van de Plaasche, Orson (2018) Relative sea-level change in Newfoundland, Canada during the past 3000 years. Quaternary Science Reviews, 201. pp. 89-110. ISSN 0277-3791 Article PeerReviewed 2018 ftunivmaynooth 2022-06-13T18:47:45Z Several processes contributing to coastal relative sea-level (RSL) change in the North Atlantic Ocean are observed and/or predicted to have distinctive spatial expressions that vary by latitude. To expand the latitudinal range of RSL records spanning the past ~3000 years and the likelihood of recognizing the characteristic fingerprints of these processes, we reconstructed RSL at two sites (Big River and Placentia) in Newfoundland from salt-marsh sediment. Bayesian transfer functions established the height of former sea level from preserved assemblages of foraminifera and testate amoebae. Age-depth models constrained by radiocarbon dates and chronohorizons estimated the timing of sediment deposition. During the past ~3000 years, RSL rose by ~3.0 m at Big River and by ~1.5 m at Placentia. A locally calibrated geotechnical model showed that post-depositional lowering through sediment compaction was minimal. To isolate and quantify contributions to RSL from global, regional linear, regional non-linear, and localscale processes, we decomposed the new reconstructions (and those in an expanded, global database) using a spatio-temporal statistical model. The global component confirms that 20th century sea-level rise occurred at the fastest, century-scale rate in over 3000 years (P > 0.999). Distinguishing the contributions from local and regional non-linear processes is made challenging by a sparse network of reconstructions. However, only a small contribution from local-scale processes is necessary to reconcile RSL reconstructions and modeled RSL trends. We identified three latitudinally-organized groups of sites that share coherent regional non-linear trends and indicate that dynamic redistribution of ocean mass by currents and/or winds was likely an important driver of sea-level change in the North Atlantic Ocean during the past ~3000 years. Article in Journal/Newspaper Newfoundland North Atlantic Maynooth University ePrints and eTheses Archive (National University of Ireland) Big River ENVELOPE(-125.196,-125.196,72.501,72.501) Canada |
institution |
Open Polar |
collection |
Maynooth University ePrints and eTheses Archive (National University of Ireland) |
op_collection_id |
ftunivmaynooth |
language |
English |
description |
Several processes contributing to coastal relative sea-level (RSL) change in the North Atlantic Ocean are observed and/or predicted to have distinctive spatial expressions that vary by latitude. To expand the latitudinal range of RSL records spanning the past ~3000 years and the likelihood of recognizing the characteristic fingerprints of these processes, we reconstructed RSL at two sites (Big River and Placentia) in Newfoundland from salt-marsh sediment. Bayesian transfer functions established the height of former sea level from preserved assemblages of foraminifera and testate amoebae. Age-depth models constrained by radiocarbon dates and chronohorizons estimated the timing of sediment deposition. During the past ~3000 years, RSL rose by ~3.0 m at Big River and by ~1.5 m at Placentia. A locally calibrated geotechnical model showed that post-depositional lowering through sediment compaction was minimal. To isolate and quantify contributions to RSL from global, regional linear, regional non-linear, and localscale processes, we decomposed the new reconstructions (and those in an expanded, global database) using a spatio-temporal statistical model. The global component confirms that 20th century sea-level rise occurred at the fastest, century-scale rate in over 3000 years (P > 0.999). Distinguishing the contributions from local and regional non-linear processes is made challenging by a sparse network of reconstructions. However, only a small contribution from local-scale processes is necessary to reconcile RSL reconstructions and modeled RSL trends. We identified three latitudinally-organized groups of sites that share coherent regional non-linear trends and indicate that dynamic redistribution of ocean mass by currents and/or winds was likely an important driver of sea-level change in the North Atlantic Ocean during the past ~3000 years. |
format |
Article in Journal/Newspaper |
author |
Kemp, Andrew C. Wright, Alexander J. Edwards, Robin J. Barnett, Robert Brain, Matthew J. Kopp, Robert E. Cahill, Niamh Horton, Benjamin P. Charman, Daniel J. Hawkes, Andrea D. Hill, Troy D. van de Plaasche, Orson |
spellingShingle |
Kemp, Andrew C. Wright, Alexander J. Edwards, Robin J. Barnett, Robert Brain, Matthew J. Kopp, Robert E. Cahill, Niamh Horton, Benjamin P. Charman, Daniel J. Hawkes, Andrea D. Hill, Troy D. van de Plaasche, Orson Relative sea-level change in Newfoundland, Canada during the past 3000 years |
author_facet |
Kemp, Andrew C. Wright, Alexander J. Edwards, Robin J. Barnett, Robert Brain, Matthew J. Kopp, Robert E. Cahill, Niamh Horton, Benjamin P. Charman, Daniel J. Hawkes, Andrea D. Hill, Troy D. van de Plaasche, Orson |
author_sort |
Kemp, Andrew C. |
title |
Relative sea-level change in Newfoundland, Canada during the past 3000 years |
title_short |
Relative sea-level change in Newfoundland, Canada during the past 3000 years |
title_full |
Relative sea-level change in Newfoundland, Canada during the past 3000 years |
title_fullStr |
Relative sea-level change in Newfoundland, Canada during the past 3000 years |
title_full_unstemmed |
Relative sea-level change in Newfoundland, Canada during the past 3000 years |
title_sort |
relative sea-level change in newfoundland, canada during the past 3000 years |
publisher |
Elsevier |
publishDate |
2018 |
url |
https://mural.maynoothuniversity.ie/13162/ https://mural.maynoothuniversity.ie/13162/1/NC_maths%26stats_relative.pdf |
long_lat |
ENVELOPE(-125.196,-125.196,72.501,72.501) |
geographic |
Big River Canada |
geographic_facet |
Big River Canada |
genre |
Newfoundland North Atlantic |
genre_facet |
Newfoundland North Atlantic |
op_relation |
https://mural.maynoothuniversity.ie/13162/1/NC_maths%26stats_relative.pdf Kemp, Andrew C. and Wright, Alexander J. and Edwards, Robin J. and Barnett, Robert and Brain, Matthew J. and Kopp, Robert E. and Cahill, Niamh and Horton, Benjamin P. and Charman, Daniel J. and Hawkes, Andrea D. and Hill, Troy D. and van de Plaasche, Orson (2018) Relative sea-level change in Newfoundland, Canada during the past 3000 years. Quaternary Science Reviews, 201. pp. 89-110. ISSN 0277-3791 |
_version_ |
1766107934179196928 |