Relative sea-level changes in Baltoscandia in the Cumbrian and early Ordovician: the predominance of tectonic factors and the absence of large scale eustatic fluctuations

2000 ◽  
Vol 320 (3-4) ◽  
pp. 375-407 ◽  
Author(s):  
E.A. Artyushkov ◽  
M. Lindström ◽  
L.E. Popov
2021 ◽  
Vol 8 (1) ◽  
Author(s):  
Yusuke Yokoyama ◽  
Anthony Purcell

AbstractPast sea-level change represents the large-scale state of global climate, reflecting the waxing and waning of global ice sheets and the corresponding effect on ocean volume. Recent developments in sampling and analytical methods enable us to more precisely reconstruct past sea-level changes using geological indicators dated by radiometric methods. However, ice-volume changes alone cannot wholly account for these observations of local, relative sea-level change because of various geophysical factors including glacio-hydro-isostatic adjustments (GIA). The mechanisms behind GIA cannot be ignored when reconstructing global ice volume, yet they remain poorly understood within the general sea-level community. In this paper, various geophysical factors affecting sea-level observations are discussed and the details and impacts of these processes on estimates of past ice volumes are introduced.


2007 ◽  
Vol 242 (1-3) ◽  
pp. 5-26 ◽  
Author(s):  
D.E. Smith ◽  
R.A. Cullingford ◽  
T.M. Mighall ◽  
J.T. Jordan ◽  
P.T. Fretwell

2011 ◽  
Vol 26 (4) ◽  
pp. 353-361 ◽  
Author(s):  
Ole Bennike ◽  
Bernd Wagner ◽  
Andreas Richter

1999 ◽  
Vol 60 (1) ◽  
pp. 83-105 ◽  
Author(s):  
Jeremy M Lloyd ◽  
Ian Shennan ◽  
Jason R. Kirby ◽  
Mairead M Rutherford

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