Composite Religiosity Scores as a Function of Condition and Number of Analytic Answers on the CRT.

<p>Number of participants answering 0, 1, 2, or 3 CRT items correctly in each condition, followed by their average religiosity composite score (with standard errors in parenthesis).</p><p>Composite Religiosity Scores as a Function of Condition and Number of Analytic Answers on the CRT.</p

Religious Beliefs as Function of Task Order and Analytic Thinking.

<p>Religious beliefs composite score as a function of task order and analytic thinking (CRT score). The solid line is the analytic first condition, whereas the dashed line is the religious beliefs first condition.</p

Regression Analysis for Analytic Thinking and Religiosity (n = 410).

<p>Regression Analysis for Analytic Thinking and Religiosity (n = 410).</p

Regression Analyses for Analytic Thinking and Religiosity, Controlling for Need for Cognition (n = 410).

<p>Regression Analyses for Analytic Thinking and Religiosity, Controlling for Need for Cognition (n = 410).</p

Sedimentology of core TMR/B.

<p>Plot of wet (grey)/dry (black) bulk density, loss-on-ignition at 105°C and 550°C, DeBroukere mean diameter, volumetric magnetic susceptibility and stratigraphic units for core TMR/B. Light gray shading represents sand beds. Dark gray shading represents no data. See text for descriptions.</p

Lidar digital terrain model of Phnom Kulen Plateau centered on Thnal Mrech dyke.

<p>Lidar digital terrain model of the main valley of Phnom Kulen Plateau with 1× vertical exaggeration. A: Thnal Srae Thbong; B: Thnal Mrech; C: NS cut bedrock; D: EW extraction lines; E: channel; F: Sediment core sampling (Imagery: Stéphane De Greef/Archaeology and Development Foundation).</p

Mineral particle size analysis of core TMR/B.

<p>Gray shading represents sand beds. Particle size classification follows the Wentworth classification scheme <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0084252#pone.0084252-Wentworth1" target="_blank">[56]</a>.</p

Pollen results (herbs, ferns).

<p>Concentration of pollen (individuals per cm³ of sediment) from herbaceous plants (dryland, wetland and aquatic), ferns, and ‘fern allies’ (<i>Selaginella</i>, Lycopodiopsida), plotted against depth/age, for core TMR/B. Closed circles represent rare taxa that did not exceed 5% of the total microfossil assemblage in any sample. Light gray shading represents sand beds. Pollen zones based on classification of the whole assemblage.</p

Pollen results (trees and shrubs).

<p>Concentration of pollen (individuals per cm³ of sediment) from trees and shrubs, plotted against depth/age, for core TMR/B. Closed circles represent rare taxa that did not exceed 5% of the total microfossil assemblage in any sample. Light gray shading represents sand beds. Pollen zones based on classification of the whole assemblage.</p

Map of central/northern Angkor and Phnom Kulen (Mahendraparvata).

<p>Contours in 10<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0084252#pone.0084252-Pottier4" target="_blank">[17]</a> and <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0084252#pone.0084252-Evans1" target="_blank">[1]</a>, topography and hydrology data from the Japan International Cooperation Agency (JICA).</p