Climatic and environmental change in Britain and Ireland during the Neolithic and Bronze Age:

2021 ◽  
pp. 547-588
Keyword(s):  
Environmental Change ◽  
Bronze Age ◽  
Climatic And Environmental Change

The land enriches the soul: On climatic and environmental change, affect, and emotional health and well-being in Rigolet, Nunatsiavut, Canada

2013 ◽  
Vol 6 ◽  
pp. 14-24 ◽  
Author(s):  
Ashlee Cunsolo Willox ◽  
Sherilee L. Harper ◽  
Victoria L. Edge ◽  
Karen Landman ◽  
Karen Houle ◽  
...  
Keyword(s):  
Environmental Change ◽  
Emotional Health ◽  
Well Being ◽  
Climatic And Environmental Change ◽  
Health And Well Being

scholarly journals The Ecology of Fencing

Africa ◽  
2008 ◽  
Vol 78 (2) ◽  
pp. 153-156 ◽  
Author(s):  
Michael J. Sheridan
Keyword(s):  
Social Science ◽  
Environmental Change ◽  
Social Relationships ◽  
Natural Science ◽  
Present Issue ◽  
Climatic And Environmental Change

In the autumn of 2004, a remarkable gathering of 102 scholars took place at St Antony's College, Oxford: they had come for an interdisciplinary symposium on ‘Trees, rain, and politics in Africa: the dynamics and politics of climatic and environmental change’. Symposium papers were grouped into panels that focused on either particular resources (such as trees and water) or particular aspects of social relationships (such as politics and discourses). This format resulted in a series of dialogues between the natural science and social science paradigms, and this first half of the present issue of Africa takes as its theme just one of those interdisciplinary conversations. Taken together, these authors demonstrate how the hybridization of natural science and social science can benefit understandings of the African past, interpretations of the African present and planning for the African future.1

scholarly journals ‘Gifts for the gods’: lake-dwellers' macabre remedies against floods in the Central European Bronze Age

Antiquity ◽  
2014 ◽  
Vol 88 (340) ◽  
pp. 456-469 ◽  
Author(s):  
Francesco Menotti ◽  
Benjamin Jennings ◽  
Hartmut Gollnisch-Moos
Keyword(s):  
Environmental Change ◽  
Bronze Age ◽  
Lake Level ◽  
Daily Life ◽  
Alpine Region ◽  
Rich Source ◽  
Late Bronze Age ◽  
Central European

The lake-dwellings of the Circum-Alpine region have long been a rich source of detailed information about daily life in Bronze Age Europe, but their location made them vulnerable to changes in climate and lake level. At several Late Bronze Age examples, skulls of children were found at the edge of the lake settlement, close to the encircling palisade. Several of the children had suffered violent deaths, through blows to the head from axes or blunt instruments. They do not appear to have been human sacrifices, but the skulls may nonetheless have been offerings to the gods by communities faced with the threat of environmental change.

scholarly journals Cliff-front aeolian and colluvial deposits, Mallorca, Western Mediterranean: a record of climatic and environmental change during the last glacial period

2001 ◽  
Vol 48 ◽  
pp. 217-232
Author(s):  
Lars B. Clemmensen ◽  
Thomas Lisborg ◽  
Richard G. Bromley ◽  
Joan J. Fornós
Keyword(s):  
Environmental Change ◽  
Environmental Changes ◽  
Western Mediterranean ◽  
Glacial Period ◽  
Last Glacial Period ◽  
Last Glacial ◽  
Aeolian Deposits ◽  
Climatic And Environmental Change ◽  
Sea Cliff ◽  
The Last Glacial

Large, cliff-front accumulations of Late Pleistocene aeolian and colluvial deposits on southeast Mallorca provide a terrestrial record of climatic and environmental change in the Western Mediterranean during the last glacial period. The cliff-front deposits are lithified and form ramps sloping toward the southeast (i.e. seaward). Radiocarbon dating suggests that the deposits formed in Oxygen Isope Stage 3, when sea level was about 50 m lower than today, and the fossil sea-cliff situated 1.5 to 2 km from the palaeo-shore. The aeolian deposits are composed of marine carbonate sand that was transported inland episodically and accumulated in embayments along the fossil sea-cliff. The sand initially formed steadily growing and forward-moving dunes, then sloping sand ramps and finally relatively small ascending dunes. Aeolian accumulation was interrupted by erosion and colluvial ramp formation, and the cliff-front sediments can be divided into two sedimentary cycles each composed of basal colluvial deposits overlain by aeolian deposits. Colluvial deposition probably records relatively humid climatic intervals, whereas aeolian accumulation probably reflects relatively arid climatic intervals. It appears that climatic and environmental changes were rapid, and it is speculated that the dynamics of the cliff-front system on Mallorca were tied to North Atlantic millennial-scale climate oscillations.

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