Skip to main content

Constructing Chronologies of Sea-Level Change from Salt-Marsh Sediments

  • Chapter
  • 551 Accesses

Part of the book series: Lecture Notes in Statistics ((LNS,volume 177))

Summary

This chapter reviews recent research into the chronology of sea-level change. Since sea-level is related to global temperatures, an understanding of sea-level change has become particularly important over recent years and is offering insights into a range of issues including ice sheet distribution, past environmental change and coastal management. In all these areas, an understanding of the timing as well as the nature of sea-level change is important and so chronometric methods as well as stratigraphic ones are typically employed. This chapter reviews the nature of the data that provide information about sea-level change and highlights some of the challenges facing those who wish to establish chronologies. The challenges have parallels with those in archaeological research, but as yet there has not been much cross-fertilization of methods between the two disciplines. This chapter offers some suggestions for the most pressing problems that still need formal tools and provides a case study using wiggle-matching that illustrates the kinds of improvements that researchers of sea-level change might expect if such methods were adopted more widely.

This is a preview of subscription content, log in via an institution.

Buying options

Chapter
USD   29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD   44.99
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD   59.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Learn about institutional subscriptions

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

References

  • Aitken, M. J.(1990).Science-based dating in archaeology. Longman, London.Allen, J. R. L. (1987a). Coal dust in the Severn Estuary, southwestern UK.Marine Pollution Bulletin, 18, 169–174

    Google Scholar 

  • Allen, J. R. L.(1987). Toward a quantitative chemostratigraphic model forsediments of late Flandrian age in the Severn Estuary, UK. SedimentaryGeology53,73–100.

    Google Scholar 

  • Allen, J.R.L(1988). Modern-period muddy sediment s in the Severn Estuary: a pollutant -based model for dating and correlation.Sedimentary Geology,58 , 1–21.

    Article  Google Scholar 

  • Allen,J.R.L.(1990a). Const raints on measurement of sea-level movementsfrom salt marsh accretion rates. Journal of the GeologicalSociety of London,147, 5–7.

    Article  Google Scholar 

  • Allen,J.R.L.(1990b).The formation of coastal peat marshes under anupward tendency of relative sea-level. Journal of the Geological Society ofLondon, 147, 743–745

    Article  Google Scholar 

  • Allen,J.R.L(1990c)Salt-marsh growth and stratificat ion; a numericalmodel with special reference to the Severn Estuary, southwest Britain.Ma-rine Geology,95, 77–96.

    Google Scholar 

  • Allen,J .R. L. (1991). Salt-marsh accretion and sea-level movement in theinner Severn Estuary, southwest Britain: the archaeological and historicalcont ribut ion. Journal of the Geological Society of London, 148, 485–494.

    Article  Google Scholar 

  • Allen, J.R.L.and Rae,J.E.(1986).Time sequence ofmetal pollution, SevernEstuary, southwestern UK. Marine Pollution Bulletin, 17, 427–431.

    Article  Google Scholar 

  • Bailiff, I. K.and Tooley, M.J.(2000).Luminescence dating of fine-grainHolocene sediments from a coastal setting. In I. Shennan and J. E.Andrews(eds.), Holocene land-ocean interaction and environmental change aroundthe western North Sea, Geological Society Special Publi cations , London,vol. 166, 55–67.

    Google Scholar 

  • Chapman, V.J.(1960).Saltmarshes and salt deserts of the world. Hill,London.

    Google Scholar 

  • Clarke,M.L.and Rendell,H.M.(2000).The development of a methodologyfor luminescence dating of Holocene sediments at the land-ocean interface.In 1. Shennan and J .E. Andrews (eds.), Holocene land-ocean interactionand environmental change around the western North Sea, GeologicalSocietySpecial Publications, London, vol. 166, 69–86

    Google Scholar 

  • Cundy, A.B.and Croudace,1.W.(1996).Sediment accretion and recentsea-level rise in the Solent, southern England - inferences from radiometricand geochemical studies. Estuarine Coastal and Shelf Science, 43, 449–467.

    Article  Google Scholar 

  • Devoy, R. J . N. (1979). Flandrian sea level changes and vegetational history ofthe lower Thames estuary. Philosophical Transactions of the Royal Societyof London, 285B, 355–410.

    Article  Google Scholar 

  • Edwards, R. J . (2001). Mid to late Holocene relative sea-level change in theHampshire Basin, UK: new data from Poole Harbour. Journal of Quater-nary Science, 16, 221–235.

    Article  Google Scholar 

  • Fairbanks R. G. (1989). A 17,000-year glacio-eustatic sea level record: influ-ence of glacial melting rates on the Younger Dryas event and deep oceancirculation. Nature,342 , 637–642.

    Article  Google Scholar 

  • Fulford, M., Champion, T. and Long, A. J. (1997). England ’s coastal heritage .Coastal Heritage and the Royal Commission on the Historical Monumentsof England, London.Gehrels, W. R.

    Google Scholar 

  • Gehrels, W. R.Belknap, D. F., Black, S.and Newham, R. M.(2002). Rapidsea-level rise in the Gulf of Maine,USA,since AD 1800. The Holocene, 12,383–389

    Google Scholar 

  • Godwin, H. (1940). Studies of the post-glacial history of the British veg-etation. III Fenland Pollen Diagrams.IV Post-glacial changes in relativeland-and sea-level in the English Fenland. Philosophical Transactions ofthe Royal Society,B570, 239–303.

    Article  Google Scholar 

  • Godwin, H. (1945). Coastal peat beds of the North sea region, as indices ofland-and sea-level changes. New Phytologist, 44 , 26–29 .Godwin, H. and Godwin, M. E. (1940). Submerged peat at Southampton -data for the study of post-glacial history V. New Phytologist, 39, 303–307.

    Google Scholar 

  • Godwin, H., Suggate, R. P. and Willis, E. H. (1958). Radiocarbon dating of the eustatic rise in ocean-level. Nature, 181, 1518–1519.

    Article  Google Scholar 

  • Gray, A. J. (1992). Saltmarsh plant ecology: zonation and succession re-visited. In J . R. L. Allen and K. Pye (eds.), Saltmarshes: morphodynam-ics, conservation and engineering significance, Cambridge University Press,Cambridge, 63–79 .

    Google Scholar 

  • Horton, B. P., Edwards , R. J. and Lloyd, J . M. (1999). A foraminiferal-basedtransfer function: implications for sea-levelstudies. Journal ofForaminiferalResearch, 29, 117–129.Research, 29, 117–129.

    Google Scholar 

  • Horton, B. P., Edwards, R. J. and Lloyd, J. M. (2000). Implications of amicrofossil transfer function in Holocene sea-level studies. In 1. Shennanand J . E. Andrews (eds.), Holocene land-ocean interaction and environ-mental change around the western North Sea, Geological Society SpecialPublications, London, vol. 166, 41–54.

    Google Scholar 

  • Kilian, M. R., van der Plicht, J. and van Geel, B. (1995). Dating raised bogs:new aspects of AMS 14C wiggle matching, a reservoir effect and climatechange. Quaternary Science Reviews, 14 , 959–966.

    Article  Google Scholar 

  • Laborel, J ., Morhange, C., Lafont, R., Le Champion, J. , Laborel-Deguen, F.and Sartoretto, S. (1994). Biological evidence of sea-level rise during thelast 4500 years on the rocky coasts of continental southwestern France andCorsica. Marine Geology, 120, 203–233.

    Article  Google Scholar 

  • Long, A. J. (1992). Coastal responses to changes in sea-level in the East KentFens and southeast England, UK over the last 7500 years. Proceedings ofthe Geologists’ Association, 103, 187–199.

    Google Scholar 

  • Long, A. J. and Roberts , D. H. (2002). A revised chronology for the FjordStade moraine in Disko Bugt, west Greenland. Journal of Quaternary Sci-ence, 17, 561–579.

    Article  Google Scholar 

  • Long, A. J., Scaife, R. G. and Edwards, R. J . (1999). Pine pollen in intertidalsediments from Poole Harbour, UK: implications for late-Holocene sedimentaccretion rates and sea-level rise. Quaternary International , 55, 3–16.

    Article  Google Scholar 

  • Long, A. J ., Scaife, R. G. and Edwards, R. J. (2000). Stratigraphic archi-tecture, relative sea-level, and models of estuary development in southernEngland: new data from Southampton Water . In K. Pye and J. R. L. Allen(eds.), Coastal and estuarine environments: sedimentology, geomorphologyand geoarchaeology , Geological Society Special Publications, London, vol.175, 253–279.

    Google Scholar 

  • Long, A. J . and Tooley, M. J . (1995). Holocene sea-level and crustal move-ments in Hampshire and Southeast England , United Kingdom. Journal ofCoastal Research, Special Issue, 17 , 299–310.

    Google Scholar 

  • Lowe, J. J. and Walker, M. J . C. (1997). Reconstructing Quaternary environ-ments . Prentice Hall, Harlow.

    Google Scholar 

  • Mastronuzzi, G. and Sanso, P. (2002). Holocene uplift rates and historicalrapid sea-level changes at the Gargano promontory, Italy. Journal of Qua-ternary Science, 17 , 593–606 .

    Article  Google Scholar 

  • Mook, W. G. and van de Plassche, O. (1986). Radiocarbon dating. InO. van de Plassche (ed.), Sea level research: a manual for the collectionand interpretation of data, Geo Books, Norwich, 525–560.

    Google Scholar 

  • Pethick, J . S. (1980). Salt marsh initiation during the Holocene transgression:the example of the north Norfolk marshes, England. Journal of Biogeogra-phy, 7, 1–9.

    Article  Google Scholar 

  • Pethick, J. S. (1981). Long-term accretion rates on tidal salt marshes. Journalof Sedimentary Petrology , 51, 571–577.

    Google Scholar 

  • Pirazzoli, P. A. (1986). Marine notches. In O. van de Plassche (ed.), Sea levelresearch: a manual for the collection and interpretation of data, Geo Books,Norwich, 361–400.

    Google Scholar 

  • Pirazzoli , P. A. (1996). Sea-level changes: the last 20,000 years. Wiley, Chich-ester.

    Google Scholar 

  • Piuto E. and Schwendt , A. E. (1997). Mathematical modeling of au-tocompaction of a Holocene transgressive valley-fill deposit, Wolfe Glade,Delaware. Geology, 25 , 57–60.

    Article  Google Scholar 

  • Pye, K. and Allen, J. R. L. (2000) . Past, present and future interactions,management challenges and research needs in coastal and estuarine envi-ronments. In K. Pye and J . R. L. Allen (eds .), Coastal and estuarine en-vironments: sedimentology, geomorphology and geoarchaeology, GeologicalSociety Special Publications, London, vol. 175, 1–4.

    Google Scholar 

  • Sawai Y., Nasu , H. and Yasuda, Y. (2002) . Fluctuations in relative ea-levelduring the past 3000 yr in the Onnetoh estuary, Hokkaido, northern Japan.Journal of Coastal Resear ch, 17, 607–622 .

    Google Scholar 

  • Scott, D. B. and Medioli, F. S. (1980) . Quantitative studies of marshforaminiferal distributions in Nova Scotia: implications for sea level studies.Cushman Foundation for Foraminiferal Research, DeKalb, Illinois .

    Google Scholar 

  • Shahidul Islam, M. and Tooley, M. J . (1999). Coastal and sea-level changesduring the Holocene in Bangladesh. Quaternary Internat ional, 55 , 61–75.

    Google Scholar 

  • Shennan, L. (1982) . Interpretation of the Flandrian sea-level data from theFenland, England. Proceedings of the Geologists Association, 93, 53–63.

    Article  Google Scholar 

  • Shennan, L. (1986) . Flandrian sea-level changes in the Fenland II: tendenciesof sea-level movement, altitudinal changes, and local and regional factors.Journal of Quaternary Science, 1, 155–179.

    Google Scholar 

  • Shennan, 1. (1994). Coastal evolution. In M. Waller (ed.), The Fenlandprojects, number 9: Flandrian environmental change in the Fenland , EastAnglian Archaeology, Cambridge, 47–84.

    Google Scholar 

  • Shennan, L. and Horton, B. P. (2002). Holocene land-and sea-level changesin Great Britain. Journal of Quaternary Research, 17,511–526.

    Google Scholar 

  • Shennan, I. , Innes, J . B., Long, A. J. and Zong, Y. (1995). Late Devensianand Holocene relative sea-level changes in northwestern Scotland: new datato test existing models. Quaternary International, 26, 97–123.

    Google Scholar 

  • Shennan, I., Lambeck, K. , Flather, R., Horton, B. , Mcarthur, J ., Innes, J. ,Lloyd, J., Rutherford, M. and Wingfield, R. (2000) . Modelling west-ern North Sea alaeogeographies and tidal changes during the Holocene.In Holocene land-ocean interaction and environmental change around theNorth Sea, Geological Society Special Publications, London, vol. 166, 299–319.

    Google Scholar 

  • Shennan, I., Tooley, M. J., Davis, M. J. and Haggart, B. A. (1983). Analysisand interpretation of Holocene sea-level data. Nature, 302, 404–406.

    Article  Google Scholar 

  • Stuiver, M., Reimer, P. J. , Bard, E., Beck, J. W., Burr, G. S., Hughen, K. A. ,Kromer , B., McCormac, F. G., Plicht, J . V. D. and Spurk, M. (1998) .IntCal98 radiocarbon age calibration, 24,000–0 cal BP . Radiocarbon, 40,1041–1083.

    Google Scholar 

  • Sutherland, D. G. (1982). Dating and associated methodological problems inthe study of Quaternary sea-level changes . In A. F. Harding (ed.), Climatechange in later prehistory, Edinburgh University Press, Edinburgh, 165–197.

    Google Scholar 

  • Switsur , R. (1994). Methods of reconstruct ion: IV. radiocarbon dating. InM. Waller (ed.) , The Fenland projects, number 9: Flandrian environmentalchange in the Fenland, East Anglian Archaeology, Cambridge, 27–34.

    Google Scholar 

  • Turney, C. S. M., Coope, G. R. , Harkness, D. D., Lowe, J . J . and Walker, M.J . C. (2000). Implicat ions for the dating ofWisconsinan (Weichselian) late-glacial events of systemat ic radiocarbon age diff erences between terrestrialplant macrofossils from a site in SW Ireland . Quaternary Research, 53,114–121.

    Google Scholar 

  • van de Plassche, O. (1982). Sea-level and water-levelmovements in the Nether-lands during the Holocene. Geological Survey of the Netherlands , Amster-dam.van de

    Google Scholar 

  • Plassche, O. (1986). Sea-level research: a manual for the collection andevaluation of data. Geo Books, Norwich.

    Google Scholar 

  • van de Plassche, O. (2000). North Atlantic climate-ocean variations and sealevel in Long Island Sound, Connect icut , since 500 cal yr AD. QuaternaryResearch, 53, 89–97 .

    Google Scholar 

  • van Geel, B. and Mook, W. G. (1989). High-resolution 14C dating of organicdeposits using natural atmospheric 14C variations. Radiocarbon, 31 , 151–156.

    Google Scholar 

  • Varekamp , J . C., Thomas, E. and van de Plassche, O. (1992). Relative sea-levelrise and climate change over the last 1500 years. Terra Nova, 4, 293–304.

    Article  Google Scholar 

  • Waller,M. (1994). Coastal evolut ion. In M.Waller (ed.), The Fenlandprojects,number 9: Flandrian environmental change in the Fenland, East AnglianAr chaeology, Cambridge, 47–84.

    Google Scholar 

Download references

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2004 Springer-Verlag London

About this chapter

Cite this chapter

Edwards, R.J. (2004). Constructing Chronologies of Sea-Level Change from Salt-Marsh Sediments. In: Buck, C.E., Millard, A.R. (eds) Tools for Constructing Chronologies. Lecture Notes in Statistics, vol 177. Springer, London. https://doi.org/10.1007/978-1-4471-0231-1_9

Download citation

  • DOI: https://doi.org/10.1007/978-1-4471-0231-1_9

  • Publisher Name: Springer, London

  • Print ISBN: 978-1-85233-763-6

  • Online ISBN: 978-1-4471-0231-1

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics