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Rapid sea-level rise in the Gulf of Maine, USA, since AD 1800

Bibliographic Data

ID12266308
AuthorsW Roland Gehrels (0000-0002-5088-5834, University of Plymouth, corresponding author), Daniel F Belknap (University of Maine), Stuart Black (0000-0003-1396-4821, Postgraduate Research Institute for Sedimentology, University of Reading, Reading RG6 6AB, UK), Rewi M Newnham (University of Plymouth), Rewi Newnham (0000-0002-6044-8945, University of Plymouth)
Year2002
Volume12
Issue4
Pages383-389
Publication date2002-05-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1191/0959683602hl555ft
OpenAlexW1998574871
LanguageEN
Citations received13
References cited24

Two sea-level records from salt marshes in coastal Maine are derived from foraminiferal analyses and AMS 14 C, 210 Pb, 137 Cs and pollen chronology. Both records cover the period from AD 800 until the present and show corresponding patterns of sea-level change when corrected for trends which could accommodate millennial-scale isostatic adjustments. The records provide a detailed sea-level chronology for the last few centuries and thus link the instrumental (tide-gauge) record with the long-term geological record of sea-level change. Results show that sea level was relatively stable between AD 800 and 1300 and reached a lowstand around AD 1800, which was preceded by an oscillation in the eighteenth century. Since AD 1800, sea levels in the Gulf of Maine have risen by 0.3-0.4 m. The onset of this rise corresponds with regional climatic warming and could be interpreted as thermal expansion of the Gulf of Maine and North Atlantic sea surface. Sea-level rise possibly slowed temporarily during the mid-nineteenth century, but twentieth-century rates are unprecedented in the last millennium and correspond with hemispheric warming

Chronology · Climate change · Climatology · Geography · North Atlantic oscillation · Period (music · Physical geography · Salt marsh · Sea level · Sea surface temperature · Tide gauge · Coastal wetland ecosystem dynamics · Geological formations and processes · Geology and Paleoclimatology Research · Geology · Oceanography · Paleontology

  • Reconstruction of recent sea-level change using testate amoebae

    Open Access•D J Charman, W Roland Gehrels et al.•Quaternary Research•2010

  • The application of foraminifera to reconstruct the rate of 20th century sea level rise, Morbihan Golfe, Brittany, France

    Open Access•Verónica Rossi, Ben Horton et al.•Quaternary Research•2011

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

    Open Access•Andrew C Kemp, Ben Horton et al.•Quaternary Research•2009

  • The use of ‘bomb spike’ calibration and high-precision AMS 14 C analyses to date salt-marsh sediments deposited during the past three centuries

    Open Access•William A Marshall, W Roland Gehrels et al.•Quaternary Research•2007

  • Two Centuries of Relative Sea-Level Rise in Dublin, Ireland, Reconstructed by Geological Tide Gauge

    Open Access•Zoë A Roseby, Katherine Southall et al.•Open Quaternary•2023

  • Expert opinion on American common eiders in eastern North America

    Open Access•Kristen Noel, Nic McLellan et al.•Socio-Ecological Practice Research•2021

  • Empowering hope-based climate change communication techniques for the Gulf of Maine

    Open Access•Aimee Bonanno, Megan Ennes et al.•Elementa Science of the…•2021

  • Distribution of foraminifera in salt marshes along the Atlantic coast of SW Europe

    Open Access•Eduardo Leorri, W Roland Gehrels et al.•Quaternary International•2010

  • Holocene aeolian morphogenetic phases in Southern Italy

    Open Access•Giuseppe Mastronuzzi, Lea Romaniello•Quaternary International•2008

  • Indigenous Archaeologies, Shell Heaps, and Climate Change

    Open Access•Bonnie Newsom, DONALD G SOCTOMAH et al.•Advances in Archaeological Practice•2023

  • Using a boundary organization approach to develop a sea level rise and storm surge impact analysis framework for coastal communities in Maine

    Open Access•Philip Camill, Maryellen Hearn et al.•Journal of Environmental Studies…•2012

  • Relative sea-level trends in New York City during the past 1500 years

    Open Access•Andrew C Kemp, Troy D Hill et al.•The Holocene•2017

  • Demographic change and shifting views about marine resources and the coastal environment in Downeast Maine

    Open Access•Thomas G Safford, L C Hamilton•Population and Environment•2012

  • Middle and Late Holocene Sea-Level Changes in Eastern Maine Reconstructed from Foraminiferal Saltmarsh Stratigraphy and AMS 14 C Dates on Basal Peat

    Open Access•W Roland Gehrels•Quaternary Research•1999

  • North Atlantic Climate–Ocean Variations and Sea Level in Long Island Sound, Connecticut, Since 500 cal yr A.D.

    Open Access•Orson van de Plassche•Quaternary Research•2000

  • Comment on “North Atlantic Climate–Ocean Variations and Sea Level in Long Island Sound, Connecticut, Since 500 cal yr A.D.”

    Open Access•Joseph T Kelley, Daniel F Belknap et al.•Quaternary Research•2001

  • Past Temperatures Directly from the Greenland Ice Sheet

    Open Access•D Dahl-Jensen, Dorthe Dahl‐Jensen et al.•Science•1998

  • Northern hemisphere temperatures during the past millennium

    Open Access•M Mann, Michael E Mann et al.•Geophysical Research Letters•1999

  • Using foraminiferal transfer functions to produce high-resolution sea-level records from salt-marsh deposits, Maine, USA

    Open Access•W Roland Gehrels•The Holocene•2000

Unique citing works13
Citations per year0,68
Citation span2007 - 2023 (17)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 9
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