Sea-Level Change and Storm-Surge Deposition in a Late Holocene Florida Salt Marsh

1998 ◽  
Vol Vol. 68 (1998), ◽  
Author(s):  
Steven L. Goodbred, Jr. (*), Eric E
1998 ◽  
Vol 68 (2) ◽  
pp. 240-252 ◽  
Author(s):  
S. L. Goodbred ◽  
E. E. Wright ◽  
A. C. Hine

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.


2001 ◽  
Vol 38 (7) ◽  
pp. 1081-1092 ◽  
Author(s):  
Gail L Chmura ◽  
Laurie L Helmer ◽  
C Beth Beecher ◽  
Elsie M Sunderland

We examine rates of salt marsh accumulation in three marshes of the outer Bay of Fundy. At each marsh we selected a site in the high marsh with similar vegetation, and thus similar elevation. Accretion rates were estimated by 137Cs, 210Pb, and pollen stratigraphy to estimate rates of change over periods of 30, 100, and ~170 years, respectively. These rates are compared with records from the two closest tide gauges (Saint John, New Brunswick, and Eastport, Maine) to assess the balance of recent marsh accretion and sea-level change. Averaged marsh accretion rates have ranged from 1.3 ± 0.4 to 4.4 ± 1.6 mm·year–1 over the last two centuries. Recent rates are similar to the rate of sea-level change recorded at Eastport, Maine, suggesting that they are in step with recent sea-level change but very sensitive to short-term variation in relative sea level. Based on the pollen stratigraphy in the marsh sediments, the marsh accretion rate was higher during the late 18th to early 19th century. Higher rates probably were due to local increases in relative sea level as a result of neotectonic activity and may have been enhanced by increased sediment deposition through ice rafting.


2019 ◽  
Vol 9 (1) ◽  
Author(s):  
Anders Schomacker ◽  
Wesley R. Farnsworth ◽  
Ólafur Ingólfsson ◽  
Lis Allaart ◽  
Lena Håkansson ◽  
...  

2019 ◽  
Vol 38 (11) ◽  
pp. 111-120
Author(s):  
Peng Xia ◽  
Xianwei Meng ◽  
Zhen Li ◽  
Pengyao Zhi ◽  
Mengwei Zhao ◽  
...  

2015 ◽  
Vol 107 ◽  
pp. 214-230 ◽  
Author(s):  
Robert L. Barnett ◽  
W. Roland Gehrels ◽  
Dan J. Charman ◽  
Margot H. Saher ◽  
William A. Marshall

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