scholarly journals Climate Variations of Summer Half-Years from the 7th to 10th Century in the Kinki Region, West Central Japan Based on Historical Documents

2010 ◽  
Vol 83 (1) ◽  
pp. 44-59 ◽  
Author(s):  
TAKASHI TANIOKA
Keyword(s):  
Historical Documents ◽  
Climate Variations ◽  
Central Japan ◽  
West Central ◽  
Summer Half

The extraterrestrial matter falls in west-central Poland (Great Poland Lowland); historical and geological data

2015 ◽  
Vol 65 (2) ◽  
pp. 273-278
Author(s):  
Wojciech T.J. Stankowski
Keyword(s):  
Indirect Evidence ◽  
Historical Documents ◽  
Geological Data ◽  
Central Poland ◽  
West Central

Abstract Direct and indirect evidence of falls of extraterrestrial matter in west-central Poland (Great Poland Lowland) is proved historically and environmentally. The chronological list of such events has historical (documents, medieval paintings, newspaper reports), geological and morphological documentation. The most important are the environmental sites of Morasko/Oborniki, Przełazy and Jankowo Dolne, where metallic meteorites were recognized. These meteorite falls represent a series of cosmic events: the Morasko fall was c. 5000 years BP, the Przełazy fall was c. 10000 years BP, and the age of the Jankowo Dolne fall is not fully documented.

Flying Back to Africa or Flying to Heaven? Competing Visions of Afterlife in the Lowcountry and Caribbean Slave Societies

2021 ◽  
Vol 31 (2) ◽  
pp. 222-261
Author(s):  
Jeroen Dewulf
Keyword(s):  
Central Africa ◽  
Historical Documents ◽  
Linguistic Research ◽  
West Central ◽  
Igbo Culture ◽  
New Interpretation ◽  
Desperate Attempt ◽  
Back To Africa

ABSTRACTThis article presents a new interpretation of the famous folktale about enslaved Africans flying home, including the legend that only those who refrained from eating salt could fly back to Africa. It rejects claims that the tale is rooted in Igbo culture and relates to suicide as a desperate attempt to escape from slavery. Rather, an analysis of historical documents in combination with ethnographic and linguistic research makes it possible to trace the tale back to West-Central Africa. It relates objections to eating salt to the Kikongo expression curia mungua (to eat salt), meaning baptism, and claims that the tale originated in the context of discussions among the enslaved about the consequences of a Christian baptism for one's spiritual afterlife.

scholarly journals Reconstruction of multi-millennial summer climate variations in central Japan by integrating tree-ring cellulose oxygen and hydrogen isotope ratios

2020 ◽  
Author(s):  
Takeshi Nakatsuka ◽  
Masaki Sano ◽  
Zhen Li ◽  
Chenxi Xu ◽  
Akane Tsushima ◽  
...  
Keyword(s):  
Time Series ◽  
Tree Ring ◽  
Isotope Ratios ◽  
Growth Effect ◽  
Climate Variations ◽  
Central Japan ◽  
The Past ◽  
Summer Climate ◽  
Age Trends ◽  
Tree Ring Cellulose

Abstract. Oxygen isotope ratios (δ18O) of tree-ring cellulose are a novel proxy of summer hydroclimate in monsoonal Asia. In central Japan, we collected 67 conifer wood samples, mainly Chamaecyparis obtusa, with ages encompassing the past 2,600 yr. The samples were taken from living old trees, excavated archeological wood, old architectural wood, and naturally buried logs. We analyzed stable isotope ratios of oxygen (δ18O) and hydrogen (δ2H) in tree-ring cellulose in these samples without using a pooling method, and constructed a statistically reliable tree-ring cellulose δ18O time-series for the past 2,500 yr. However, there were distinct age trends and level offsets in the δ18O record, and cellulose δ18O values showed a gradual decrease as an individual tree matures. This suggested it is difficult to establish a cellulose δ18O chronology for low-frequency signals by simple averaging of all the δ18O time-series data. However, there were opposite age trends in the cellulose δ2H, and δ2H gradually increased with tree age. There were clear positive correlations in the short periodicity variations between δ18O and δ2H, probably indicating a common climate signal. A comparison of the δ18O and δ2H time-series in individual trees with tree-ring width suggested that the opposite age trends of δ18O and δ2H are caused by temporal changes in the degree of post-photosynthetic isotope exchange with xylem water, accompanied by changes in stem growth rate (growth effect) that are influenced by human activity in the forests of central Japan. Based on the assumptions that cellulose δ18O and δ2H vary positively and negatively with constant proportional coefficients due to climate variations and the growth effect, respectively, we solved simultaneous equations for the climatological and physiological components of variations in tree-ring cellulose δ18O and δ2H in order to remove the age trend (growth effect). This enabled us to evaluate the climatic record from cellulose δ18O variations. The extracted climatological component in the cellulose δ18O for the past 2,600 yr in central Japan was well correlated with numerous instrumental, historical, and paleoclimatological records of past summer climate at various spatial and temporal scales. This indicates that integration of tree-ring cellulose δ18O and δ2H data is a promising method to reconstruct past summer climate variations on annual to millennial time-scales, irrespective of the growth affect. However, analytical and statistical methods need to be improved for further development of this climate proxy.

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