Sedimentary and sea level changes during glacial cycles and their control on glacimarine facies architecture

1990 ◽  
Vol 53 (1) ◽  
pp. 15-52 ◽  
Author(s):  
G. S. Boulton
2020 ◽  
Author(s):  
Sean J Buckley ◽  
Chris Brauer ◽  
Peter Unmack ◽  
Michael Hammer ◽  
Luciano B. Beheregaray

ABSTRACTWhile the influence of Pleistocene climatic changes on divergence and speciation has been well-documented across the globe, complex spatial interactions between hydrology and eustatics over longer timeframes may also determine species evolutionary trajectories. Within the Australian continent, glacial cycles were not associated with changes in ice cover and instead largely resulted in fluctuations from moist to arid conditions across the landscape. Here, we investigate the role of hydrological and coastal topographic changes brought about by Plio-Pleistocene climatic changes on the biogeographic history of a small Australian freshwater fish, the southern pygmy perch Nannoperca australis. Using 7,958 ddRAD-seq (double digest restriction-site associated DNA) loci and 45,104 filtered SNPs, we combined phylogenetic, coalescent and species distribution analyses to investigate the relative roles of aridification, sea level and tectonics and their associated biogeographic changes across southeast Australia. Sea-level changes since the Pliocene and reduction or disappearance of large waterbodies throughout the Pleistocene were determining factors in strong divergence across the clade, including the initial formation and maintenance of a cryptic species, N. ‘flindersi’. Isolated climatic refugia and fragmentation due to lack of connected waterways maintained the identity and divergence of inter- and intraspecific lineages. Our historical findings suggest that predicted increases in aridification and sea level due to anthropogenic climate change might result in markedly different demographic impacts, both spatially and across different landscape types.


2007 ◽  
Vol 247 (3-4) ◽  
pp. 357-381 ◽  
Author(s):  
F. Fluteau ◽  
Gilles Ramstein ◽  
Jean Besse ◽  
R. Guiraud ◽  
J.P Masse

2000 ◽  
Vol 178 (1) ◽  
pp. 147-176 ◽  
Author(s):  
M. R. House ◽  
V. V. Menner ◽  
R. T. Becker ◽  
G. Klapper ◽  
N. S. Ovnatanova ◽  
...  

2008 ◽  
Vol 23 (1) ◽  
pp. n/a-n/a ◽  
Author(s):  
Eva Moreno ◽  
Franck Bassinot ◽  
François Baudin ◽  
Marie-Thérèse Vénec-Peyré

1999 ◽  
Vol 18 (14) ◽  
pp. 1681-1695 ◽  
Author(s):  
G. Cabioch ◽  
L.F. Montaggioni ◽  
G. Faure ◽  
A. Ribaud-Laurenti

2021 ◽  
Author(s):  
Gustav Pallisgaard-Olesen ◽  
Vivi Kathrine Pedersen ◽  
Natalya Gomez

<div> <p>The landscape in western Scandinavia has undergone dramatic changes through numerous glaciations during the Quaternary. These changes in topography and in the volumes of offshore sediment deposits, have caused significant isostatic adjustments and local sea level changes, owing to erosional unloading and depositional loading of the lithosphere. Mass redistribution from erosion and deposition also has the potential to cause significant pertubations of the geoid, resulting in additional sea-level changes. The combined sea-level response from these processes, is yet to be investigated in detail for Scandinavia.</p> </div><div> <p>In this study we estimate the total sea level change from late-Pliocene- Quaternary glacial erosion and deposition in the Scandinavian region, using a gravitationally self-consistent global sea level model that includes the full viscoelastic response of the solid Earth to surface loading and unloading. In addition to the total late Pliocene-Quaternary mass redistribution, we <span>also </span>estimate transient sea level changes related specifically to the two latest glacial cycles.</p> </div><div> <p>We utilize existing observations of offshore sediment thicknesses of glacial origin, and combine these with estimates of onshore glacial erosion and estimates of erosion on the inner shelf. Based on these estimates, we can define mass redistribution and construct a preglacial landscape setting.</p> </div><div> <p>Our preliminary results show <span>perturbations of</span> the local sea level up to ∼ 200 m since<span> the</span> late-Pliocene in the Norwegian Sea, suggesting that erosion and deposition ha<span>ve</span> influenced the local paleo sea level history in Scandinavia significantly.</p> </div>


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