scholarly journals Corrigendum

The Holocene ◽  
2014 ◽  
Vol 24 (11) ◽  
pp. 1634-1635

Kitamura A and Kobayashi K (2014) Geologic evidence for prehistoric tsunamis and coseismic uplift during the ad 1854 Ansei-Tokai earthquake in Holocene sediments on the Shimizu Plain, central Japan. The Holocene 24(7): 814–827. DOI: 10.1177/0959683614530447 . In this article, Figure 3 is incomplete. The correct figure is shown below.

The Holocene ◽  
2011 ◽  
Vol 22 (7) ◽  
pp. 793-800 ◽  
Author(s):  
Ryota Okunaka ◽  
Tatsuichiro Kawano ◽  
Jun Inoue

Phytolith and macroscopic charcoal in cumulative soils on the Soni Plateau, Central Japan, were evaluated to clarify the Holocene history of intentional fires and grassland development, and to compare the findings with those derived from pollen and charcoal records in sediments taken from a nearby mire in the previous study. Prior to ~1500 cal. BP, Bambusoid short-cell phytoliths and Pleioblastus-type and Bambusoideae-type bulliform cell phytoliths were abundant with scarce charcoal particles (<1000 particles/cm3). In contrast, since ~1500 cal. BP Andropogoneae-type bulliform cell phytoliths and Bilobate short-cell phytoliths were dominant with abundant charcoal particles (>1000 particles/cm3). Based on correlating these records with pollen and charcoal records in mire sediments, prior to ~1500 cal. BP, dwarf bamboo flourished on the forest floor under largely fire-free conditions, whereas since ~1500 cal. BP, grassland dominated by Japanese pampas grass has been sustained by periodic intentional burning that has continued until the present day.


2015 ◽  
Vol 53 (10) ◽  
pp. 903-921 ◽  
Author(s):  
V. N. Melenevskii ◽  
G. A. Leonova ◽  
V. A. Bobrov ◽  
V. A. Kashirtsev ◽  
S. K. Krivonogov

2021 ◽  
Vol 62 ◽  
pp. 101148
Author(s):  
Deke Xu ◽  
Houyuan Lu ◽  
Chunsheng Jin ◽  
Zhaoyan Gu ◽  
Xinxin Zuo ◽  
...  

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