Relative sea-level change in Newfoundland, Canada during the past ∼3000 years

Autor: Robert L. Barnett, Andrew C. Kemp, Andrea D. Hawkes, Alexander J. Wright, Matthew J. Brain, Robert E. Kopp, Orson van de Plassche, Robin J. Edwards, Benjamin P. Horton, Niamh Cahill, Troy D. Hill, Dan J. Charman

Publikováno v: Kemp, A C, Wright, A J, Edwards, R J, Barnett, R L, Brain, M J, Kopp, R E, Cahill, N, Horton, B P, Charman, D J, Hawkes, A D, Hill, T D & van de Plassche, O 2018, ' Relative sea-level change in Newfoundland, Canada during the past ∼3000 years ', Quaternary Science Reviews, vol. 201, pp. 89-110 . https://doi.org/10.1016/j.quascirev.2018.10.012
Quaternary science reviews, 2018, Vol.201, pp.89-110 [Peer Reviewed Journal]
Quaternary Science Reviews, 201, 89-110. Elsevier Limited

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

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::589ecf2c4c7cac0208bca15947a74326
https://doi.org/10.1016/j.quascirev.2018.10.012

Estimating tectonic uplift of the Cape Fear Arch (south-eastern United States) using reconstructions of Holocene relative sea level

Autor: Andrew C. Kemp, Benjamin P. Horton, Simon E. Engelhart, Alexander J. Wright, Robert E. Kopp, David J. Mallinson, Orson van de Plassche

Publikováno v: Journal of Quaternary Science. 29:749-759

We use relative sea-level (RSL) reconstructions and a spatiotemporal statistical model to estimate the rate of uplift of the Cape Fear Arch, a Mesozoic structural high, during the last � 4000 years. We reconstructed RSL using 12 radiocarbon-dated s

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::dd9fa54366b4853c39a3aed04907d760
https://doi.org/10.1002/jqs.2746

The relative utility of foraminifera and diatoms for reconstructing late Holocene relative sea-level change in North Carolina, USA

Autor: Stephen J. Culver, Orson van de Plassche, D. Reide Corbett, Benjamin P. Horton, Andrew C. Kemp, Robin J. Edwards

Publikováno v: Quaternary Research, 71, 9-21. Academic Press Inc.
Kemp, A C, Horton, B P, Corbett, R, Culver, S J, Edwards, R J & van de Plassche, O 2009, ' The relative utility of foraminifera and diatoms for reconstructing late Holocene relative sea-level change in North Carolina, USA ', Quaternary Research, vol. 71, pp. 9-21 . https://doi.org/10.1016/j.yqres.2008.08.007

Foraminifera and diatoms preserved in salt-marsh sediments have been used to produce high-resolution records of Holocene relative sea-level (RSL) change. To determine which of these microfossil groups is most appropriate for this purpose we investiga

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f04ddc15e04ff8aa5fff782f378f864f
https://research.vu.nl/en/publications/5adc03bd-9e11-4e66-aca0-4733a9ac3e9f

North Atlantic climate-ocean variations and sea level in Long Island Sound, Connecticut, since 500 cal yr A.D

Autor: Orson van de Plassche

Publikováno v: Quaternary Research, 53, 89-97. Academic Press Inc.
van de Plassche, O 2001, ' North Atlantic climate-ocean variations and sea level in Long Island Sound, Connecticut, since 500 cal yr A.D. ', Quaternary Research, vol. 53, pp. 89-97 . https://doi.org/10.1006/qres.1999.2099

A record of detrended mean high water (MHW) variations from Hammock River marsh, Connecticut, is extended from ca. 850 to ca. 500 cal yr A.D. and correlated with summer-temperature reconstructions from northern Fennoscandia and northern Eurasia, Gree

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e3c15d7b641d66791757b8075f114793
https://hdl.handle.net/1871/29645

Optical dating of dune sand for the study of sea-level change

Autor: Orson van de Plassche, Ronald K. Lubberts, D. J. Huntley, Sytze van Heteren

Publikováno v: van Heteren, S, Huntley, D J, van de Plassche, O & Lubberts, R K 2000, ' Optical dating of dune sand for the study of sea-level change. ', Geology, vol. 28, no. 5, pp. 411-415 . https://doi.org/10.1130/0091-7613(2000)28<411:ODODSF>2.0.CO;2
Geology, 28(5), 411-415. Geological Society of America

A new, widely applicable method to obtain well-constrained relative sea-level records, presented here, relies on optical dating of inorganic coastal landforms and sediments. Eighteen optical ages of basal dune sand from a barrier in Massachusetts, Un

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b69e9536e543aea043af5b909e270f90
https://hdl.handle.net/1871.1/7b0e02fa-f922-4dd9-a350-31e64c9be76e