Matches in SemOpenAlex for { <https://semopenalex.org/work/W2057429163> ?p ?o ?g. }
- W2057429163 endingPage "110" @default.
- W2057429163 startingPage "90" @default.
- W2057429163 abstract "Abstract Understanding late Holocene to present relative sea-level changes at centennial or sub-centennial scales requires geological records that dovetail with the instrumental era. Salt marsh sediments are one of the most reliable geological tide gauges. In this paper we review the methodological and technical advances that promoted research on ‘high resolution’ late Holocene sea-level change. We work through an example to demonstrate different pathways to quantitative reconstructions of relative sea level based on salt marsh sediments. We demonstrate that any reconstruction is in part a result of the environment from which the record is taken, the modern dataset used to calibrate the fossil changes, statistical assumptions behind calibrating microfossil assemblages and choices made by the researchers. With the error term of typical transfer function models ~ 10–15% of the tidal range, micro-tidal environments should produce the most precise sea-level reconstructions. Sampled elevation range of the modern dataset also has a strong influence on model predictive ability. Model-specific errors may under represent total uncertainty which comes from field practices, sedimentary environment, palaeo-tidal changes and sediment compaction as well as statistical uncertainties. Geological tide gauges require a detailed chronology but we must be certain that apparent relative sea-level fluctuations are not simply a consequence of an age–depth model. We make six suggestions to aid the development and interpretation of geological tide gauge records." @default.
- W2057429163 created "2016-06-24" @default.
- W2057429163 creator A5001929892 @default.
- W2057429163 creator A5009262493 @default.
- W2057429163 creator A5015302018 @default.
- W2057429163 creator A5049669987 @default.
- W2057429163 creator A5063266063 @default.
- W2057429163 creator A5083387810 @default.
- W2057429163 creator A5090102294 @default.
- W2057429163 date "2013-07-01" @default.
- W2057429163 modified "2023-10-16" @default.
- W2057429163 title "Salt marshes as late Holocene tide gauges" @default.
- W2057429163 cites W1494081909 @default.
- W2057429163 cites W1548333476 @default.
- W2057429163 cites W1575688672 @default.
- W2057429163 cites W1963846006 @default.
- W2057429163 cites W1963947392 @default.
- W2057429163 cites W1964286915 @default.
- W2057429163 cites W1965967607 @default.
- W2057429163 cites W1966852422 @default.
- W2057429163 cites W1971112759 @default.
- W2057429163 cites W1971414220 @default.
- W2057429163 cites W1977661041 @default.
- W2057429163 cites W1978248369 @default.
- W2057429163 cites W1978912552 @default.
- W2057429163 cites W1981594027 @default.
- W2057429163 cites W1983523307 @default.
- W2057429163 cites W1983758393 @default.
- W2057429163 cites W1985202776 @default.
- W2057429163 cites W1986103123 @default.
- W2057429163 cites W1986968352 @default.
- W2057429163 cites W1987806181 @default.
- W2057429163 cites W1988347634 @default.
- W2057429163 cites W1988598673 @default.
- W2057429163 cites W1988817083 @default.
- W2057429163 cites W1989199095 @default.
- W2057429163 cites W1990020115 @default.
- W2057429163 cites W1990477265 @default.
- W2057429163 cites W1990639855 @default.
- W2057429163 cites W1991318196 @default.
- W2057429163 cites W1992278565 @default.
- W2057429163 cites W1995637978 @default.
- W2057429163 cites W1997452875 @default.
- W2057429163 cites W1998697563 @default.
- W2057429163 cites W1998867744 @default.
- W2057429163 cites W1999797075 @default.
- W2057429163 cites W2001261279 @default.
- W2057429163 cites W2002054363 @default.
- W2057429163 cites W2002494458 @default.
- W2057429163 cites W2003764094 @default.
- W2057429163 cites W2006357786 @default.
- W2057429163 cites W2007782885 @default.
- W2057429163 cites W2008358083 @default.
- W2057429163 cites W2009721490 @default.
- W2057429163 cites W2011110941 @default.
- W2057429163 cites W2014663788 @default.
- W2057429163 cites W2015846537 @default.
- W2057429163 cites W2016007157 @default.
- W2057429163 cites W2016709223 @default.
- W2057429163 cites W2020766810 @default.
- W2057429163 cites W2023137308 @default.
- W2057429163 cites W2026895911 @default.
- W2057429163 cites W2028167494 @default.
- W2057429163 cites W2028200333 @default.
- W2057429163 cites W2029822818 @default.
- W2057429163 cites W2030904424 @default.
- W2057429163 cites W2035185206 @default.
- W2057429163 cites W2035407089 @default.
- W2057429163 cites W2037099692 @default.
- W2057429163 cites W2037950848 @default.
- W2057429163 cites W2041529744 @default.
- W2057429163 cites W2042554483 @default.
- W2057429163 cites W2042584557 @default.
- W2057429163 cites W2043817944 @default.
- W2057429163 cites W2043832652 @default.
- W2057429163 cites W2045707843 @default.
- W2057429163 cites W2046179515 @default.
- W2057429163 cites W2046809970 @default.
- W2057429163 cites W2047786034 @default.
- W2057429163 cites W2047789448 @default.
- W2057429163 cites W2048223029 @default.
- W2057429163 cites W2053795842 @default.
- W2057429163 cites W2057314456 @default.
- W2057429163 cites W2058597995 @default.
- W2057429163 cites W2058861125 @default.
- W2057429163 cites W2058981126 @default.
- W2057429163 cites W2059516882 @default.
- W2057429163 cites W2059674544 @default.
- W2057429163 cites W2062125548 @default.
- W2057429163 cites W2062359768 @default.
- W2057429163 cites W2062362025 @default.
- W2057429163 cites W2063472329 @default.
- W2057429163 cites W2064536940 @default.
- W2057429163 cites W2070370342 @default.
- W2057429163 cites W2070549462 @default.
- W2057429163 cites W2071909497 @default.
- W2057429163 cites W2073660985 @default.
- W2057429163 cites W2076016862 @default.