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Salt Marsh Zonal Migration and Ecosystem Service Change in Response to Global Sea Level Rise: A Case Study from an Urban Region Ecology and Society
Feagin, Rusty A; Texas A&M University; feaginr@tamu.edu; Costanza, Robert; University of Vermont; rcostanz@uvm.edu.
Coastal wetland plants are expected to respond to global sea level rise by migrating toward higher elevations. Housing, infrastructure, and other anthropogenic modifications are expected to limit the space available for this potential migration. Here, we explore the ecological and economic effects of projected Intergovernmental Panel on Climate Change (IPCC) 2007 report sea level changes at the plant community scale using the highest horizontal (1 m) and vertical (0.01 m) resolution data available, using a 6 x 6 km area as an example. Our findings show that salt marshes do not always lose land with increasing rates of sea level rise. We found that the lower bound of the IPCC 2007 potential rise (0.18 m by 2095) actually increased the total marsh area....
Tipo: Peer-Reviewed Reports Palavras-chave: Coastal ecology; Coastal plant migration; Sea level rise; Spatial analysis.
Ano: 2010
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Rapid sea level rise and ice sheet response to 8,200-year climate event ArchiMer
Cronin, T. M.; Vogt, P. R.; Willard, D. A.; Thunell, R.; Halka, J.; Berke, M.; Pohlman, J..
The largest abrupt climatic reversal of the Holocene interglacial, the cooling event 8.6 - 8.2 thousand years ago (ka), was probably caused by catastrophic release of glacial Lake Agassiz-Ojibway, which slowed Atlantic meridional overturning circulation (AMOC) and cooled global climate. Geophysical surveys and sediment cores from Chesapeake Bay reveal the pattern of sea level rise during this event. Sea level rose similar to 14 m between 9.5 to 7.5 ka, a pattern consistent with coral records and the ICE- 5G glacio-isostatic adjustment model. There were two distinct periods at similar to 8.9 - 8.8 and similar to 8.2 - 7.6 ka when Chesapeake marshes were drown as sea level rose rapidly at least similar to 12 mm yr(-1). The latter event occurred after the 8.6...
Tipo: Text Palavras-chave: Sea level rise; Holocene; 8.2 ka event.
Ano: 2007 URL: https://archimer.ifremer.fr/doc/00235/34644/33009.pdf
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Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum ArchiMer
Mackintosh, Andrew N.; Verleyen, Elie; O'Brien, Philip E.; White, Duanne A.; Jones, R. Selwyn; Mckay, Robert; Dunbar, Robert; Gore, Damian B.; Fink, David; Post, Alexandra L.; Miura, Hideki; Leventer, Amy; Goodwin, Ian; Hodgson, Dominic A.; Lilly, Katherine; Crosta, Xavier; Golledge, Nicholas R.; Wagner, Bernd; Berg, Sonja; Van Ommen, Tas; Zwartz, Dan; Roberts, Stephen J.; Vyverman, Wim; Masse, Guillaume.
The East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Earth, and documenting its evolution since the Last Glacial Maximum (LGM) is important for understanding its present-day and future behaviour. As part of a community effort, we review geological evidence from East Antarctica that constrains the ice sheet history throughout this period (similar to 30,000 years ago to present). This includes terrestrial cosmogenic nuclide dates from previously glaciated regions, C-14 chronologies from glacial and post-glacial deposits onshore and on the continental shelf, and ice sheet thickness changes inferred from ice cores and continental-scale ice sheet models. We also include new C-14 dates from the George V Land Terre Adelie Coast shelf. We...
Tipo: Text Palavras-chave: Antarctica; Last Glacial Maximum; Ice sheet; Sea level rise.
Ano: 2014 URL: https://archimer.ifremer.fr/doc/00290/40085/39171.pdf
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The evolution of a Holocene banner bank controlled by morphodynamics and structural setting of a macrotidal coast: Saint-Brieuc Bay (NW-EUROPE) ArchiMer
Traoré, Kalil; Menier, David; Gensac, Erwan; Le Roy, Pascal; Lambert, Clément; Bessin, Paul; Pédoja, Kevin; Duperret, Anne; Le Gall, Romain.
The morphology and internal structure of the Horaine Bank (Bay of Saint-Brieuc, NW France) are described based on multibeam echosounder and high-resolution seismic datasets coupled with vibro-core data. The Horaine Bank shows large-scale bedforms in the lee of a submerged rocky shoal, which allowed defining it as a Banner Bank. The internal structure of the sandbank reveals four seismic units (U1–U4) on a Cambrian basement (U0). The basal unit U1 is interpreted as reworked lowstand fluvial sediments those infilled micro incised valleys during a rise in sea level. This unit is overlain by paleo-coastal barrier sand-spit (U2) whose development was controlled by swell in the context of a rapid rise in sea level. The successive prograding unit (U3) is...
Tipo: Text Palavras-chave: Sand banks; Banner bank; Holocene climate; Geomorphology; Sea level rise; Tidal gyre..
Ano: 2021 URL: https://archimer.ifremer.fr/doc/00685/79660/82424.pdf
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Coastal dynamics under conditions of rapid sea-level rise: Late Pleistocene to Early Holocene evolution of barrier-lagoon systems on the northern Adriatic shelf (Italy) ArchiMer
Storms, J; Weltje, G; Terra, G; Cattaneo, Antonio; Trincardi, F.
This multidisciplinary case study of two preserved barrier systems combined the analysis of radiocarbon datings, grain-size distributions, high-resolution seismics, and shelf bathymetry with reconstructions of palaeo-environmental conditions (tides, waves, sea-level change) and forward modelling of barrier-lagoon systems, to provide an integrated view of the coastal transgressive evolution of a large sector of the northern Adriatic shelf between 15 and 8 ka BR Palaeo-environmental reconstructions point to increased tidal amplitude, low-energy wave climate and high rates of sea-level rise (up to 60 mm/a) during the formation of the oldest preserved barrier system (similar to 90 m water depth; 14.3 cal ka BP). A younger barrier system (42 m water depth; 10.5...
Tipo: Text Palavras-chave: Progressive sorting; Forward modelling; Tidal amplification; Barrier lagoon system; Transgression; Sea level rise.
Ano: 2008 URL: http://archimer.ifremer.fr/doc/2008/publication-4473.pdf
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Effects of ocean warming, eutrophication and salinity variations on the growth of habitat-forming macroalgae in estuarine environments Acta Botanica
Borburema,Henrique Douglas dos Santos; Lima,Ruth Pessoa de; Miranda,George Emmanuel Cavalcanti de.
ABSTRACT Global change and coastal eutrophication are affecting macroalgae worldwide. We analyzed the effects of increased water temperature (25, 28 and 32 °C) and eutrophication on the growth of Bostrychia binderi and Bostrychia montagnei in a range of salinities (18, 24, 30, 36 and 42 PSU) through three independent multifactorial experiments. Both species had higher growth at 25 °C than at 28 and 32 °C (warming scenario projected by IPCC), suggesting a negative effect of ocean warming. The species showed a broad tolerance to the range of salinities tested, with higher growth at 36 and 42 PSU, as a local adaptation strategy. Oligotrophic seawater significantly affected the growth of both species because the lowest growth was found in this condition,...
Tipo: Info:eu-repo/semantics/article Palavras-chave: Bostrychia; Bostrychietum; Climate change; Ecophysiology; Estuarine macroalgae; Eutrophication; Global change; Growth; Salinity variation; Sea level rise.
Ano: 2020 URL: http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-33062020000400662
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Sea-land limits: a case study Anais da ABC (AABC)
Mesquita,Afranio R. de; Blitzkow,Denizar; França,Carlos A. S.; Trabanco,Jorge L. A.; Corrêa,Marco A.; Monteiro,Mauro Q..
The limits between sea and land were estimated at "Pulso" beach located in the Southeastern Brazilian shelf (φ = 23°33/17.4886"S; Λ = 045° 13'13.0504"W - WGS84), between the island of São Sebastião and the city of Ubatuba, SP, Brazil. The relative sea level of the year 1831 at "Pulso" beach, as per Brazilian law Number 9760 dated from 1946, was estimated and materialized. The retro-estimation allowed the demarcation of the Legal Sea-Land Limits at "Pulso" beach as per the terms of the law. The accuracy of the procedure for the transference of the long-term sea level from the research station of Ubatuba to "Pulso" beach was assessed by parallel work of geometrical leveling referred to the IBGE (Brazilian Institute of Geography and Statistics) geodetic...
Tipo: Info:eu-repo/semantics/article Palavras-chave: Relative Sea Level; Brazilian law; Sea-Land Limits; "Pulso" beach; Geodetic leveling; Southeastern Brazilian shelf; Global warming; Sea level rise.
Ano: 2011 URL: http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652011000400009
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Coastal vulnerability to sea level rise in the southwestern Colombian Caribbean Boletín de Investigaciones
García Echavarría,Luz Marleny; Alcántara-Carrió,Javier; Jaramillo Vélez,Alfredo.
ABSTRACT One of the concerns about climate change is the rise in sea level, which is associated with an increase in coastal erosion, saline intrusion in estuaries and the risk of flooding. These changes make it necessary to evaluate the coastal susceptibility and its adaptation capacity facing with this phenomenon. The Coastal Vulnerability Index made up of the variables geomorphology, slope, rate of change of coastline, significant wave height, rate of change of relative sea level and mean tidal range, seeks to locally estimate vulnerability. This work focused on determining the Vulnerability in the coastline of the sectors Volcán de Lodo, Río Hobo, Zapata and Punta Las Vacas through the use of aerial photographs, satellite images, in situ data and...
Tipo: Info:eu-repo/semantics/article Palavras-chave: Susceptibility; Climate change; Sea level rise; Coastal erosion..
Ano: 2022 URL: http://www.scielo.org.co/scielo.php?script=sci_arttext&pid=S0122-97612022000200009
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