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1

Rovere, Alessio, Paolo Stocchi, and Matteo Vacchi. "Eustatic and Relative Sea Level Changes." Current Climate Change Reports 2, no. 4 (2016): 221–31. http://dx.doi.org/10.1007/s40641-016-0045-7.

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2

Creel, Roger C., Jacqueline Austermann, Nicole S. Khan, et al. "Postglacial relative sea level change in Norway." Quaternary Science Reviews 282 (April 2022): 107422. http://dx.doi.org/10.1016/j.quascirev.2022.107422.

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3

Ingebritsen, S. E., and D. L. Galloway. "Coastal subsidence and relative sea level rise." Environmental Research Letters 9, no. 9 (2014): 091002. http://dx.doi.org/10.1088/1748-9326/9/9/091002.

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4

Antonioli, Fabrizio, Sanja Faivre, Luigi Ferranti, and Carmelo Monaco. "Tectonic contribution to relative sea level change." Quaternary International 232, no. 1-2 (2011): 1–4. http://dx.doi.org/10.1016/j.quaint.2010.10.003.

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5

Rosentau, Alar, Volker Klemann, Ole Bennike, et al. "A Holocene relative sea-level database for the Baltic Sea." Quaternary Science Reviews 266 (August 2021): 107071. http://dx.doi.org/10.1016/j.quascirev.2021.107071.

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6

Hoffmann, Gösta, Nico Schmedemann, and Maria-Theresia Schafmeister. "Relative sea-level curve for SE Rügen and Usedom Island (SW Baltic Sea coast, Germany) using decompacted profiles." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 160, no. 1 (2009): 69–78. http://dx.doi.org/10.1127/1860-1804/2009/0160-0069.

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7

Uścinowicz, Szymon. "A relative sea-level curve for the Polish Southern Baltic Sea." Quaternary International 145-146 (March 2006): 86–105. http://dx.doi.org/10.1016/j.quaint.2005.07.007.

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8

Bungenstock, Friederike, and Henk J. T. Weerts. "Holocene relative sea-level curves for the German North sea coast." International Journal of Earth Sciences 101, no. 4 (2011): 1083–90. http://dx.doi.org/10.1007/s00531-011-0698-3.

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9

Jeon, Dong-Chull. "Relative Sea-level Change Around the Korean Peninsula." Ocean and Polar Research 30, no. 4 (2008): 373–78. http://dx.doi.org/10.4217/opr.2008.30.4.373.

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10

Husson, Laurent, and Clinton P. Conrad. "Tectonic velocities, dynamic topography, and relative sea level." Geophysical Research Letters 33, no. 18 (2006): n/a. http://dx.doi.org/10.1029/2006gl026834.

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11

Nijhuis, A. G., D. A. Edmonds, R. L. Caldwell, et al. "Fluvio-deltaic avulsions during relative sea-level fall." Geology 43, no. 8 (2015): 719–22. http://dx.doi.org/10.1130/g36788.1.

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12

Martínez, Sergio, and Alejandra Rojas. "Relative sea level during the Holocene in Uruguay." Palaeogeography, Palaeoclimatology, Palaeoecology 374 (March 2013): 123–31. http://dx.doi.org/10.1016/j.palaeo.2013.01.010.

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13

Shaw, John, and Donald L. Forbes. "The postglacial relative sea-level lowstand in Newfoundland." Canadian Journal of Earth Sciences 32, no. 9 (1995): 1308–30. http://dx.doi.org/10.1139/e95-107.

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Relative sea level in coastal regions of Newfoundland fell from late-glacial maximum levels to postglacial minima in several phases: (i) an early period of high relative sea level, when Late Wisconsinan ice was at the coast and discharging meltwater plumes into the ocean; (ii) a period of rapidly falling relative sea level, during which glaciers retreated inland; and (iii) a period without glacier ice, during which relative sea level continued to fall, but at decreasing rates. Falling relative sea level caused fluvial incision of glacial deposits in some coastal embayments, and culminated with
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14

Day, J. W., A. Rismondo, F. Scarton, D. Are, and G. Cecconi. "Relative sea level rise and Venice lagoon wetlands." Journal of Coastal Conservation 4, no. 1 (1998): 27–34. http://dx.doi.org/10.1007/bf02806486.

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15

Mesquita, Afrânio Rubens de, Carlos Augusto De Sampaio França, Denizard Blitzkow, Marco Antonio Corrêa, Jorge Luiz Alves Trabanco, and Mauro Quandt Monteiro. "UNION SEA LAND PROPERTY AND THE RELATIVE 1831 SEA LEVEL AT BARRA DO UNA BEACH." Revista Brasileira de Geofísica 31, no. 5 (2013): 11. http://dx.doi.org/10.22564/rbgf.v31i5.385.

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ABSTRACT. Measurements of relative sea level have been performed at Barra do Una (BU) located on the Southern Brazilian coast near the Island of São Sebastião, in São Paulo State, Brazil, relative to the sea level in 1831, as established by law n. 9760, 1946. The estimate took into account three plausible hypotheses about the change in global relative sea level from 1831 to the present and allowed to establish the “Terrenos de Marinha” on BU. The motivation behind this work, the hypothesesand the methods used are described, along a brief history of the “Terrenos de Marinha”. The discussion of
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16

Nicholls, Robert J., and Stephen P. Leatherman. "Adapting to sea‐level rise: Relative sea‐level trends to 2100 for the United States." Coastal Management 24, no. 4 (1996): 301–24. http://dx.doi.org/10.1080/08920759609362298.

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17

., Jamaluddin, Romuald Sohores, and Muhammad Fawzy Ismullah. "RELATIONSHIP BETWEEN SEQUENCE STRATIGRAPHY AND RELATIVE SEA-LEVEL CHANGES." JURNAL GEOCELEBES 1, no. 2 (2017): 38. http://dx.doi.org/10.20956/geocelebes.v1i2.2293.

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The continuous sea-level rise will result in conditions where the level of accommodation space is greater than that of sediment supply produced undertransgression conditions. When the sea level reaches its maximum point, the sedimentation rate will exceed the sea level rise and aggrades becomes more dominant progradation will result in new Highstand System Tract (HST) condition. Keyword: Accommodation, Sea level changes, Sedimentation, Sequence, Stratigraphy
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18

Dickman, S. R. "[Comment on “Changes in relative sea level”] Changes in sea level: The question of secular motion." Eos, Transactions American Geophysical Union 67, no. 18 (1986): 447. http://dx.doi.org/10.1029/eo067i018p00447-01.

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19

Mesquita, Afrânio Rubens de, Alberto Dos Santos Franco, Joseph Harari, and Carlos Augusto De Sampaio França. "ON SEA LEVEL ALONG THE BRAZILIAN COAST." Revista Brasileira de Geofísica 31, no. 5 (2013): 33. http://dx.doi.org/10.22564/rbgf.v31i5.387.

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ABSTRACT. This is Part II of a contribution on Brazilian sea levels – Part I dealt with the seasonal variability. It examines the sea level changes along the Brazilian coast from series with less than 40 years of measurement, against the background of changes in series of all continents and islands around the world, considering data distributed by the Permanent Service for Mean Sea Level (PSMSL). The method of analysis follows the display of the data in a: 1) first plot of relative sea level trends (C), against the length of the series (L) expressed in years and a: 2) second plot showing the re
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20

Hassan, Kamaludin, Suzannah Akmal, and Yongqiang Zong. "Late Holocene relative low sea level at Merang, Terengganu." Bulletin of the Geological Society of Malaysia 62 (December 1, 2016): 23–29. http://dx.doi.org/10.7186/bgsm62201604.

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21

Chekhovich, Petr. "RELATIVE SEA-LEVEL CHANGES:A SURFACE EXPRESSION OF DEEP PROCESSES." LIFE OF THE EARTH 44, no. 1 (2022): 4–19. http://dx.doi.org/10.29003/m2616.0514-7468.2022_44_1/4-19.

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The article presents an overview of current ideas about the possible causes and physical mechanisms of relative sea-level changes. The choice of the predominant factor can be demonstrated by the study of stratigraphic sequences formed at the oceanic basin margins or in the epeiric seas of cratonic interior areas. Such studies lead to the conclusion that high frequency fluctuations with a period of less than 1 Myr are caused primarily by the glacial episodes on the land. Fluctuations with a longer period of 1-3 Myr are controlled by intraplate tectonic processes, among which the prograde metamo
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22

Burgess, Peter M. "Modeling carbonate sequence development without relative sea-level oscillations." Geology 29, no. 12 (2001): 1127. http://dx.doi.org/10.1130/0091-7613(2001)029<1127:mcsdwr>2.0.co;2.

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23

Tosi, Luigi, Cristina Da Lio, Sandra Donnici, Tazio Strozzi, and Pietro Teatini. "Vulnerability of Venice's coastland to relative sea-level rise." Proceedings of the International Association of Hydrological Sciences 382 (April 22, 2020): 689–95. http://dx.doi.org/10.5194/piahs-382-689-2020.

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Abstract. Relative sea-level rise (RSLR), i.e. sea-level rise due to climate changes combined with land subsidence, is one of the processes that is most severely threatening the coastal systems around the world. The Venice coastland forms the major low-lying area in Italy and encompasses a variety of environments, such as farmlands, estuaries, deltas, lagoons and urbanized areas. Valuable ecosystems, historical heritages and economic activities are located in this area. Since most of the territory lies at a ground elevation below or slightly above the mean sea-level, also a few mm yr−1 of land
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24

Woodroffe, C. D., K. Rogers, K. L. McKee, C. E. Lovelock, I. A. Mendelssohn, and N. Saintilan. "Mangrove Sedimentation and Response to Relative Sea-Level Rise." Annual Review of Marine Science 8, no. 1 (2016): 243–66. http://dx.doi.org/10.1146/annurev-marine-122414-034025.

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25

Rashid, Towhida, S. Suzuki, Hiroshi Sato, M. H. Monsur, and S. K. Saha. "Relative sea-level changes during the Holocene in Bangladesh." Journal of Asian Earth Sciences 64 (March 2013): 136–50. http://dx.doi.org/10.1016/j.jseaes.2012.12.007.

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26

List, Jeffrey H., Asbury H. Sallenger, Mark E. Hansen, and Bruce E. Jaffe. "Accelerated relative sea-level rise and rapid coastal erosion:." Marine Geology 140, no. 3-4 (1997): 347–65. http://dx.doi.org/10.1016/s0025-3227(97)00035-2.

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27

HAGGART, B. ANDREW. "Relative sea-level change in the Beauly Firth, Scotland." Boreas 15, no. 2 (2008): 191–207. http://dx.doi.org/10.1111/j.1502-3885.1986.tb00083.x.

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28

Hawkins, Rhys, Laurent Husson, Gaël Choblet, Thomas Bodin, and Julia Pfeffer. "Virtual Tide Gauges for Predicting Relative Sea Level Rise." Journal of Geophysical Research: Solid Earth 124, no. 12 (2019): 13367–91. http://dx.doi.org/10.1029/2019jb017943.

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29

Avsar, N. B., and S. H. Kutoglu. "RELATIVE SEA LEVEL CHANGE ALONG THE BLACK SEA COAST FROM TIDE-GAUGE OBSERVATIONS." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLII-3/W8 (August 20, 2019): 43–47. http://dx.doi.org/10.5194/isprs-archives-xlii-3-w8-43-2019.

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&lt;p&gt;&lt;strong&gt;Abstract.&lt;/strong&gt; Potential sea level rise poses a significant threat to low-lying areas. Considering present and future of coastal areas, scientific study of sea level rise is an essential for adapting to sea level extremes. In this study, the relative sea level change in the Black Sea were investigated using data of 12 tide-gauge and 6 GNSS stations. Results generally indicated sea level rise along the Black Sea coast. Only at Bourgas tide-gauge station, a sea level fall was detected. A significant sea level change were not determined at Sinop tide-gauge station
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30

LEE, Han Soo, and Arata KANEKO. "Regional Projection of Relative Sea Level Rise in the Seto Inland Sea, Japan." Journal of Japan Society of Civil Engineers, Ser. B2 (Coastal Engineering) 70, no. 2 (2014): I_1276—I_1280. http://dx.doi.org/10.2208/kaigan.70.i_1276.

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31

Bechor, Benny, Theotokis Theodoulou, Giorgio Spada, Silas Dean, and Dorit Sivan. "Medieval relative low sea-level indications from the Peloponnese and the Aegean Sea." Quaternary International 545 (April 2020): 17–27. http://dx.doi.org/10.1016/j.quaint.2019.11.026.

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32

Vacchi, Matteo, Alessio Rovere, Alexandros Chatzipetros, Nickolas Zouros, and Marco Firpo. "An updated database of Holocene relative sea level changes in NE Aegean Sea." Quaternary International 328-329 (April 2014): 301–10. http://dx.doi.org/10.1016/j.quaint.2013.08.036.

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33

Meijles, Erik W., Patrick Kiden, Harm-Jan Streurman, et al. "Holocene relative mean sea-level changes in the Wadden Sea area, northern Netherlands." Journal of Quaternary Science 33, no. 8 (2018): 905–23. http://dx.doi.org/10.1002/jqs.3068.

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34

Rushby, Greg T., Geoff T. Richards, W. Roland Gehrels, William P. Anderson, Mark D. Bateman, and William H. Blake. "Testing the mid-Holocene relative sea-level highstand hypothesis in North Wales, UK." Holocene 29, no. 9 (2019): 1491–502. http://dx.doi.org/10.1177/0959683619854513.

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Accurate Holocene relative sea-level curves are vital for modelling future sea-level changes, particularly in regions where relative sea-level changes are dominated by isostatically induced vertical land movements. In North Wales, various glacial isostatic adjustment (GIA) models predict a mid-Holocene relative sea-level highstand between 4 and 6 ka, which is unsubstantiated by any geological sea-level data but affects the ability of geophysical models to model accurately past and future sea levels. Here, we use a newly developed foraminifera-based sea-level transfer function to produce a 3300
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35

Gehrels, W. Roland, David A. Dawson, Jon Shaw, and William A. Marshall. "Using Holocene relative sea-level data to inform future sea-level predictions: An example from southwest England." Global and Planetary Change 78, no. 3-4 (2011): 116–26. http://dx.doi.org/10.1016/j.gloplacha.2011.05.013.

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36

Hede, Signe Ulfeldt. "Prehistoric settlements and Holocene relative sea-level changes in northwest Sjælland, Denmark." Bulletin of the Geological Society of Denmark 50 (December 15, 2003): 141–49. http://dx.doi.org/10.37570/bgsd-2003-50-11.

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The topographic and geographic distribution of the Mesolithic and Neolithic habitations seen today in the Saltbæk Vig area, north-west Sjælland are directly related to relative sea-level changes of the Littorina Sea. The archaeological data indicate that the settlements changed their topographic positions from lower to higher ground. This pattern is explained by a rising relative sea-level during the Atlantic and early Subboreal period. Geological investigations of this phenomenon focused on changes in relative sea-level documented by the sedimentary record. At Smakkerup Huse, a late Mesolithi
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37

Smith, D. E., and R. A. Cullingford. "Flandrian relative sea-level changes in the Montrose Basin area." Scottish Geographical Journal 101, no. 2 (1985): 91–104. http://dx.doi.org/10.1080/14702548508554960.

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38

Muto, Tetsuji. "How to reconstruct changing rates of relative sea-level rise." Journal of the Sedimentological Society of Japan 47, no. 47 (1998): 83–93. http://dx.doi.org/10.4096/jssj1995.47.83.

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39

Stocchi, Paolo, Carlota Escutia, Alexander J. P. Houben, et al. "Relative sea-level rise around East Antarctica during Oligocene glaciation." Nature Geoscience 6, no. 5 (2013): 380–84. http://dx.doi.org/10.1038/ngeo1783.

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40

Nakada, M., and K. Lambeck. "Glacial rebound and relative sea-level variations: a new appraisal." Geophysical Journal International 90, no. 1 (1987): 171–224. http://dx.doi.org/10.1111/j.1365-246x.1987.tb00680.x.

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41

Carter, W. E. "Reply [to “Comment on ‘Changes in relative mean sea level’”]." Eos, Transactions American Geophysical Union 67, no. 18 (1986): 447. http://dx.doi.org/10.1029/eo067i018p00447-02.

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42

Smith, D. E., and R. A. Cullingford. "Flandrian relative sea‐level changes in the Montrose basin area." Scottish Geographical Magazine 101, no. 2 (1985): 91–105. http://dx.doi.org/10.1080/00369228518736623.

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43

Peltier, W. R., and Rosemarie Drummond. "A “broad-shelf effect” upon postglacial relative sea level history." Geophysical Research Letters 29, no. 8 (2002): 10–1. http://dx.doi.org/10.1029/2001gl014273.

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44

Morhange, Christophe, Paolo A. Pirazzoli, Nick Marriner, Lucien F. Montaggioni, and Tanios Nammour. "Late Holocene relative sea-level changes in Lebanon, Eastern Mediterranean." Marine Geology 230, no. 1-2 (2006): 99–114. http://dx.doi.org/10.1016/j.margeo.2006.04.003.

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45

Mei‐E, Ren. "Relative sea level rise in China and its socioeconomic implications." Marine Geodesy 17, no. 1 (1994): 37–44. http://dx.doi.org/10.1080/15210609409379708.

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46

Vacchi, Matteo, Simon E. Engelhart, Daria Nikitina, et al. "Postglacial relative sea-level histories along the eastern Canadian coastline." Quaternary Science Reviews 201 (December 2018): 124–46. http://dx.doi.org/10.1016/j.quascirev.2018.09.043.

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47

Lloyd, Jeremy M., Ian Shennan, Jason R. Kirby, and Mairead M. Rutherford. "Holocene relative sea-level changes in the inner Solway Firth." Quaternary International 60, no. 1 (1999): 83–105. http://dx.doi.org/10.1016/s1040-6182(99)00009-9.

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48

Edwards, R. J., and B. P. Horton. "Reconstructing relative sea-level change using UK salt-marsh foraminifera." Marine Geology 169, no. 1-2 (2000): 41–56. http://dx.doi.org/10.1016/s0025-3227(00)00078-5.

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49

Nichols, Maynard M. "Sediment accumulation rates and relative sea-level rise in lagoons." Marine Geology 88, no. 3-4 (1989): 201–19. http://dx.doi.org/10.1016/0025-3227(89)90098-4.

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50

LIVERMAN, DAVID G. E. "Relative sea-level history and isostatic rebound in Newfoundland, Canada." Boreas 23, no. 3 (2008): 217–30. http://dx.doi.org/10.1111/j.1502-3885.1994.tb00944.x.

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