The severity of drought weather condition during the demise of the Maya civilisation almost i M years agone has been quantified, representing some other slice of bear witness that could live used to solve the longstanding mystery of what caused the downfall of i of the ancient world's peachy civilisations.
Edzná ruins, Campeche. Pictured is the 31 m tall Pirámide de los Cinco Pisos (pyramid of the v storeys), located inwards the Great Plaza [Credit: Nick Evans] |
Based on these measurements, the researchers establish that annual atmospheric precipitation decreased betwixt 41% together with 54% during the menses of the Maya civilisation's collapse, amongst periods of upwards to 70% rainfall reduction during peak drought conditions, together with that relative humidity declined past times 2% to 7% compared to today. The results are reported inwards the journal Science.
"The purpose of climate alter inwards the collapse of Classic Maya civilisation is somewhat controversial, partly because previous records are express to qualitative reconstructions, for illustration whether weather condition were wetter or drier," said Nick Evans, a PhD pupil inwards Cambridge's Department of public Sciences together with the paper's starting fourth dimension author. "Our study represents a substantial advance every bit it provides statistically robust estimates of rainfall together with humidity levels during the Maya downfall."
During the ninth century however, at that spot was a major political collapse inwards the cardinal Maya region: their famous limestone cities were abandoned together with dynasties ended. And spell the Maya people survived beyond this period, their political together with economical ability was depleted.
There are multiple theories every bit to what caused the collapse of the Maya civilisation, such every bit invasion, war, environmental degradation together with collapsing merchandise routes. In the 1990s, however, researchers were able to slice together climate records for the menses of the Maya collapse, together with establish that it correlated amongst an extended menses of extreme drought.
Now, Hodell together with his colleagues convey applied a novel method together with estimated the extent of this drought. Using a novel geochemical method to stair out the H2O locked inside gypsum from Chichancanab, the researchers convey built a consummate model of hydrological weather condition during the final Classic Period when the Maya collapsed.
The researchers analysed the dissimilar isotopes of H2O trapped inside the crystal construction of the gypsum to produce upwards one's hear changes inwards rainfall together with relative humidity during the Maya downfall.
In periods of drought, to a greater extent than H2O evaporates from lakes such every bit Chichancanab, together with because the lighter isotopes of H2O evaporate faster, the H2O becomes heavier. Influenza A virus subtype H5N1 higher proportion of the heavier isotopes, such every bit oxygen-18 together with hydrogen-2 (deuterium), would thus dot drought conditions. By mapping the proportion of the dissimilar isotopes contained inside each layer of gypsum, the researchers were able to build a model to approximate past times changes inwards rainfall together with relative humidity over the menses of the Maya collapse.
This quantitative climate information tin flame live used to amend predict how these drought weather condition may convey affected agriculture, including yields of the Maya's staple crops, such every bit maize.
Source: University of Cambridge [August 02, 2018]
Sumber http://archaeologynewsnetwork.blogspot.com
Buat lebih berguna, kongsi: