Late Holocene sea-level fall and turn-off of reef flat carbonate production: Rethinking bucket fill and coral reef growth models

Geology ◽  
2015 ◽  
Vol 43 (2) ◽  
pp. 175-178 ◽  
Author(s):  
Daniel L. Harris ◽  
Jody M. Webster ◽  
Ana Vila-Concejo ◽  
Quan Hua ◽  
Yusuke Yokoyama ◽  
...  
Coral Reefs ◽  
2008 ◽  
Vol 27 (4) ◽  
pp. 991-996 ◽  
Author(s):  
M. S. Engels ◽  
C. H. Fletcher ◽  
M. Field ◽  
C. L. Conger ◽  
C. Bochicchio

Coral Reefs ◽  
1998 ◽  
Vol 17 (3) ◽  
pp. 273-276 ◽  
Author(s):  
T. P. Scoffin ◽  
M. D. A. Le Tissier

2017 ◽  
Author(s):  
David J. Mallinson ◽  
◽  
Stephen J. Culver ◽  
Eduardo Leorri ◽  
Ryan Mulligan

2021 ◽  
pp. 102002
Author(s):  
Toshiaki Irizuki ◽  
Jun Takahashi ◽  
Koji Seto ◽  
Hiroaki Ishiga ◽  
Yuki Fujihara ◽  
...  

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.


Nature ◽  
2018 ◽  
Vol 558 (7710) ◽  
pp. 396-400 ◽  
Author(s):  
Chris T. Perry ◽  
Lorenzo Alvarez-Filip ◽  
Nicholas A. J. Graham ◽  
Peter J. Mumby ◽  
Shaun K. Wilson ◽  
...  

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