4.7 Article

Extended late Holocene relative sea-level histories for North Carolina, USA

Journal

QUATERNARY SCIENCE REVIEWS
Volume 160, Issue -, Pages 13-30

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quascirev.2017.01.012

Keywords

Foraminifera; Gulf Stream; Tidal-range change; Salt marsh

Funding

  1. NSF [OCE-1458921, EAR-1402017, EAR-1322742, OCE-1130843, OCE-1458904]
  2. USGS Climate and Land Use RD program
  3. Directorate For Geosciences
  4. Division Of Earth Sciences [1322658, 1428975, 1440015] Funding Source: National Science Foundation
  5. Division Of Earth Sciences
  6. Directorate For Geosciences [1402017, 1322742] Funding Source: National Science Foundation
  7. Division Of Ocean Sciences
  8. Directorate For Geosciences [1458921, 1458904] Funding Source: National Science Foundation

Ask authors/readers for more resources

produced similar to 3000-year long relative sea-level (RSL) histories for two sites in North Carolina (USA) using foraminifera preserved in new and existing cores of dated salt-marsh sediment. At Cedar Island, RSL rose by similar to 2.4 m during the past similar to 3000 years compared to similar to 3.3 m at Roanoke Island. This spatial difference arises primarily from differential GIA that caused late Holocene RSL rise to be 0.1-0.2 mm/yr faster at Roanoke Island than at Cedar Island. However, a non-linear difference in RSL between the two study regions (particularly from similar to 0 CE to similar to 1250 CE) indicates that additional local-to regional-scale processes drove centennial-scale RSL change in North Carolina. Therefore, the Cedar Island and Roanoke Island records should be considered as independent of one another. Between-site differences on sub-millennial timescales cannot be adequately explained by non-stationary tides, sediment compaction, or local sediment dynamics. We propose that a period of accelerating RSL rise from similar to 600 CE to 1100 CE that is present at Roanoke Island (and other sites north of Cape Hatteras at least as far as Connecticut), but absent at Cedar Island (and other sites south of Cape Hatteras at least as far as northeastern Florida) is a local-to regional-scale effect of dynamic ocean and/or atmospheric circulation. (C) 2017 Elsevier Ltd. All rights reserved.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

Article Geosciences, Multidisciplinary

Minimal stratigraphic evidence for coseismic coastal subsidence during 2000 yr of megathrust earthquakes at the central Cascadia subduction zone

Alan R. Nelson, Andrea D. Hawkes, Yuki Sawai, Ben P. Horton, Rob C. Witter, Lee-Ann Bradley, Niamh Cahill

Summary: The lithology and microfossil biostratigraphy beneath the marshes of a central Oregon estuary provide evidence that rules out more than 0.5 meters of coseismic coastal subsidence during the past 2000 years. The presence of multiple peat-mud contacts in cores and outcrops, often considered to be related to subsidence during megathrust earthquakes, could not be confirmed to have formed during great earthquakes. The study suggests that only the youngest peat-mud contact is likely associated with the 1700 CE Cascadia earthquake, while the rest may be related to gradual changes in tide levels.

GEOSPHERE (2021)

Correction Geosciences, Multidisciplinary

Relative sea-level stability and the radiocarbon marine reservoir correction at Natuna Island, Indonesia, since 6400 yr BP (vol 430, 106342, 2020)

Jeannette Xiu Wen Wan, Aron J. Meltzner, Adam D. Switzer, Ke Lin, Xianfeng Wang, Sarah L. Bradley, Danny H. Natawidjaja, Bambang W. Suwargadi, Benjamin P. Horton

MARINE GEOLOGY (2021)

Article Geography, Physical

Examining the role of solar activity, climate, and the socio-historical context in high all-cause mortality (northern Portugal, 1700-1880)

Joao Moreno, Filipa Moreno, Francisco Fatela, Eduardo Leorri

Summary: The study examined the influence of solar activity on climate and all-cause mortality, finding that peaks in mortality rates were associated with wars, famines, and other factors triggered by climate deterioration. Wavelet transform coherence analysis revealed (multi)decadal oscillations in total solar irradiance and North Atlantic Oscillation, suggesting a potential role of space weather in modulating mortality dynamics.

BOREAS (2022)

Article Geography, Physical

Fluvial and coastal landform changes in the Aceh River delta (northern Sumatra) during the century leading to the 2004 Indian Ocean tsunami

Stoil Chapkanski, Gilles Brocard, Franck Lavigne, Camille Tricot, Ella Meilianda, Nazli Ismail, Jedrzej Majewski, Jean-Philippe Goiran, Dedy Alfian, Patrick Daly, Benjamin Horton, Adam Switzer, Veronique Degroot, Annika Steuer, Bernhard Siemon, Julien Cavero, Clement Virmoux, Darusman Darusman

Summary: River deltas are significantly impacted by demographic growth and land use intensification, leading to rapid migration of coastal areas and threats to urban settlements, coastal farming, and ecosystems. Studying the geomorphological evolution of deltas can be enhanced through the use of overlapping maps and aerial photographs, along with satellite images, to track changes in fluvial and coastal landforms. The evolution of river channels and coastlines in the Aceh River delta over the past 130 years reveals a progressive decrease in sediment supply, resulting in lengthening and narrowing of river channels, landward migration of the shoreline, and narrowing of beach ridges. The 2004 Indian Ocean tsunami caused an instantaneous retreat of the coastline, accelerating the overall trend of retreat. Beach ridges located up-drift of rivers and tidal channel mouths are particularly vulnerable to long-term landward retreat and tsunamigenic erosion.

EARTH SURFACE PROCESSES AND LANDFORMS (2022)

Editorial Material Geosciences, Multidisciplinary

Reply to: Atlantic circulation change still uncertain

L. Caesar, G. D. McCarthy, D. J. R. Thornalley, N. Cahill, S. Rahmstorf

NATURE GEOSCIENCE (2022)

Article Multidisciplinary Sciences

Timing of emergence of modern rates of sea-level rise by 1863

Jennifer S. Walker, Robert E. Kopp, Christopher M. Little, Benjamin P. Horton

Summary: Sea-level rise is an important indicator of climate changes. The authors estimate that global sea-level rise emerged by 1863 and find spatial variability of emergence at sites within the North Atlantic.

NATURE COMMUNICATIONS (2022)

Article Geography, Physical

The giant 1960 tsunami in the context of a 6000-year record of paleotsunamis and coastal evolution in south-central Chile

Pedro Matos-Llavona, Lisa L. Ely, Breanyn MacInnes, Tina Dura, Marco A. Cisternas, Joanne Bourgeois, David Bruce, Jessica DePaolis, Alexander Dolcimascolo, Benjamin P. Horton, Daniel Melnick, Alan R. Nelson, Walter Szeliga, Robert L. Wesson

Summary: This study examines the inconsistency between the tsunami deposits at a location in south-central Chile and the historical and geological records of tsunamis. The research suggests that the discrepancy may be attributed to factors such as falling sea levels, coastal geomorphological changes, and a potentially larger tsunami in 1960.

EARTH SURFACE PROCESSES AND LANDFORMS (2022)

Article Geosciences, Multidisciplinary

The response of foraminifera to rapid sea-level rise from tidal restoration of Ni-les'tun marsh, Oregon, USA

Yvonne Milker, Tina Dura, Benjamin P. Horton

Summary: This study examines the response of foraminifera to rapid changes in relative sea-level (RSL) using observations from the tidal restoration of Ni-les'tun marsh over a six-year period. The findings suggest that foraminifera show a delayed colonization of new habitats following RSL changes, potentially due to their reproductive cycle and limited food availability. However, postdepositional taphonomic processes have minimal influence on the similarity between modern and fossil assemblages.

MARINE GEOLOGY (2022)

Article Geography, Physical

Reproducibility and variability of earthquake subsidence estimates from saltmarshes of a Cascadia estuary

Jason S. Padgett, Simon E. Engelhart, Harvey M. Kelsey, Robert C. Witter, Niamh Cahill

Summary: This study examines fossil foraminiferal assemblages to assess sudden relative sea level changes in northern Humboldt Bay, California. The results reveal significant variability in subsidence stratigraphy across an estuary. The study also highlights the importance of multiple microfossil reconstructions from different marsh sites to account for estimation variability and enhance confidence in vertical coseismic deformation estimates.

JOURNAL OF QUATERNARY SCIENCE (2022)

Article Environmental Sciences

A Bayesian time series model for reconstructing hydroclimate from multiple proxies

Niamh Cahill, Jacky Croke, Micheline Campbell, Kate Hughes, John Vitkovsky, Jack Eaton Kilgallen, Andrew Parnell

Summary: We propose a Bayesian model for probabilistic reconstructions of hydroclimatic variability in Queensland Australia using multiple palaeoclimate proxy records. The model combines time-series modeling with inverse prediction to reconstruct the hydroclimate back through time. Case studies for Brisbane and Fitzroy catchments show the probability of extreme hydroclimate behavior beyond the observed instrumental period.

ENVIRONMETRICS (2023)

Article Geography, Physical

A 5000-year record of relative sea-level change in New Jersey, USA

Jennifer S. Walker, Tanghua Li, Timothy A. Shaw, Niamh Cahill, Donald C. Barber, Matthew J. Brain, Robert E. Kopp, Adam D. Switzer, Benjamin P. Horton

Summary: Stratigraphic data from salt marshes accurately reconstruct Holocene relative sea-level change and provide necessary constraints to glacial isostatic adjustment models. A new record of Mid- to Late-Holocene sea-level rise is presented using basal peats from a salt marsh in New Jersey. The sea-level index points range from 1211 to 4414 years BP, and the average rate of sea-level rise from 5000 years BP to present is 1.7 +/- 0.1 mm/year. Comparisons with GIA models show the models tend to overestimate sea-level rise in the past 5000 years.

HOLOCENE (2023)

Article Environmental Sciences

Global survey shows planners use widely varying sea-level rise projections for coastal adaptation

Daniella Hirschfeld, David Behar, Robert J. Nicholls, Niamh Cahill, Thomas James, Benjamin P. Horton, Michelle E. Portman, Rob Bell, Matthew Campo, Miguel Esteban, Bronwyn Goble, Munsur Rahman, Kwasi Appeaning Addo, Faiz Ahmed Chundeli, Monique Aunger, Orly Babitsky, Anders Beal, Ray Boyle, Jiayi Fang, Amir Gohar, Susan Hanson, Saul Karamesines, M. J. Kim, Hilary Lohmann, Kathy McInnes, Nobuo Mimura, Doug Ramsay, Landis Wenger, Hiromune Yokoki

Summary: Including sea-level rise (SLR) projections in coastal adaptation planning is crucial, but only 72% of coastal practitioners currently utilize them, with lower utilization in developing countries. There is no global standard in the use of SLR projections, but countries with histories of adaptation and consistent national support show greater assimilation of SLR projections.

COMMUNICATIONS EARTH & ENVIRONMENT (2023)

Article Environmental Sciences

Deglacial perspectives of future sea level for Singapore

Timothy A. Shaw, Tanghua Li, Trina Ng, Niamh Cahill, Stephen Chua, Jedrzej M. Majewski, Yudhishthra Nathan, Gregory G. Garner, Robert E. Kopp, Till J. J. Hanebuth, Adam D. Switzer, Benjamin P. Horton

Summary: Low elevation equatorial and tropical coastal regions are at high risk due to sea level rise. Based on regional geological reconstructions and instrumental records, we provide probability perspectives of future sea level for Singapore. The quantification of sea-level change reveals that during the last deglaciation, sea level rose by approximately 121 m and had an average rate of 15 mm/yr, resulting in a reduction of the paleogeographic landscape by about 2.3 million km(2). Projections suggest that under a moderate emissions scenario, sea level is expected to rise by 0.95 m at a rate of 7.3 mm/yr by 2150, which has only been exceeded during rapid ice mass loss events similar to 14.5 and similar to 9 thousand years ago. However, projections under a high emissions scenario incorporating uncertain ice-sheet processes have no precedent during the last deglaciation.

COMMUNICATIONS EARTH & ENVIRONMENT (2023)

No Data Available