scholarly journals SOME DATA ON THE HOLOCENE SEA-LEVEL CHANGES IN THE SENDAI COASTAL PLAIN, NORTHERN JAPAN

1978 ◽  
Vol 51 (2) ◽  
pp. 158-175 ◽  
Author(s):  
Kunio OMOTO ◽  
Yasushi OUCHI
Radiocarbon ◽  
1980 ◽  
Vol 22 (3) ◽  
pp. 695-704 ◽  
Author(s):  
Mebus A Geyh

The limits of the statistical evaluation of14C dates by histograms are discussed. The method of the attempt to establish a global chronology of the short-term eustatic sea-level changes during the Holocene is examined as well as its correlation with the precisely determined Suess wiggles.


Palaeoworld ◽  
2011 ◽  
Vol 20 (1) ◽  
pp. 92-97 ◽  
Author(s):  
Subhendu Bardhan ◽  
Tuhin Ghosh ◽  
Subhronil Mondal ◽  
Arindam Roy ◽  
Sumanta Mallick

Author(s):  
Martina Karle ◽  
Friederike Bungenstock ◽  
Achim Wehrmann

Abstract The Holocene sea-level rise has led to significant changes in present-day coastal zones through multifold retrogradational and slightly progradational displacements of the mainland coastline. During the course of this postglacial transgression, sediments characteristic of coastal environments accumulated first in palaeovalleys of the pre-Holocene landscape and later on the subsequently developed coastal plain. Based on a compilation of sedimentological, lithological and litho-chronostratigraphical data of more than 1200 sediment cores, we generated four palaeogeographic maps of the coastal zone of the central Wadden Sea to document with a high spatial resolution the landscape changes during characteristic phases of the Holocene sea-level rise, i.e. the periods 8600–6500 cal BP, 6500–2700 cal BP, 2700–1500 cal BP and 1500–1000 cal BP. Along three cross-sections, representing different hydrodynamic conditions and exposure, we exemplify how the Holocene landscape development and sedimentary facies types are controlled by the local palaeorelief, sea-level changes, sediment supply, accommodation space, the morphodynamic impact of channel shifts, and their erosion base. This leads to a better understanding of main factors controlling the local depositional processes of the coastal landscape along the central Wadden Sea during the Holocene transgression.


Author(s):  
Nikolay Esin ◽  
Nikolay Esin ◽  
Vladimir Ocherednik ◽  
Vladimir Ocherednik

A mathematical model describing the change in the Black Sea level depending on the Aegean Sea level changes is presented in the article. Calculations have shown that the level of the Black Sea has been repeating the course of the Aegean Sea level for the last at least 6,000 years. And the level of the Black Sea above the Aegean Sea level in the tens of centimeters for this period of time.


2013 ◽  
Vol 13 (4) ◽  
pp. 141-152 ◽  
Author(s):  
Kenitiro Suguio ◽  
Alcina Magnуlia Franco Barreto ◽  
Paulo Eduardo de Oliveira ◽  
Francisco Hilário Rego Bezerra ◽  
Maria Cristina Santiago Hussein Vilela

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