scholarly journals Early Stages of Sea-Level Rise Lead To Decreased Salt Marsh Plant Diversity through Stronger Competition in Mediterranean-Climate Marshes

PLoS ONE ◽  
2017 ◽  
Vol 12 (1) ◽  
pp. e0169056 ◽  
Author(s):  
Akana E. Noto ◽  
Jonathan B. Shurin
2014 ◽  
Vol 148 (1) ◽  
pp. 5-18
Author(s):  
Antoine Meirland ◽  
Emilie Gallet-Moron ◽  
Hervé Rybarczyk ◽  
Frédéric Dubois ◽  
Olivier Chabrerie

2017 ◽  
Vol 28 (6) ◽  
pp. 1178-1186 ◽  
Author(s):  
Pedro Daleo ◽  
Juan Alberti ◽  
Carlos Martín Bruschetti ◽  
Paulina Martinetto ◽  
Jesús Pascual ◽  
...  

Author(s):  
Amy K. Langston ◽  
Clark R. Alexander ◽  
Merryl Alber ◽  
Matthew L. Kirwan

2012 ◽  
Vol 102 ◽  
pp. 65-70 ◽  
Author(s):  
Teddy Baumberger ◽  
François Mesléard ◽  
Thomas Croze ◽  
Laurence Affre

2007 ◽  
Vol 44 (10) ◽  
pp. 1453-1465 ◽  
Author(s):  
Julia F Daly ◽  
Daniel F Belknap ◽  
Joseph T Kelley ◽  
Trevor Bell

Differential sea-level change in formerly glaciated areas is predicted owing to variability in extent and timing of glacial coverage. Newfoundland is situated close to the margin of the former Laurentide ice sheet, and the orientation of the shoreline affords the opportunity to investigate variable rates and magnitudes of sea-level change. Analysis of salt-marsh records at four sites around the island yields late Holocene sea-level trends. These trends indicate differential sea-level change in recent millennia. A north–south geographic trend reflects submergence in the south, very slow sea-level rise in the northeast, and a recent transition from falling to rising sea-level at the base of the Northern Peninsula. This variability is best explained as a continued isostatic response to deglaciation.


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