2013
DOI: 10.1111/1556-4029.12169
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Seasonal Variation of Carcass Decomposition and Gravesoil Chemistry in a Cold (Dfa) Climate

Abstract: It is well known that temperature significantly affects corpse decomposition. Yet relatively few taphonomy studies investigate the effects of seasonality on decomposition. Here, we propose the use of the Köppen-Geiger climate classification system and describe the decomposition of swine (Sus scrofa domesticus) carcasses during the summer and winter near Lincoln, Nebraska, USA. Decomposition was scored, and gravesoil chemistry (total carbon, total nitrogen, ninhydrin-reactive nitrogen, ammonium, nitrate, and so… Show more

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Cited by 70 publications
(64 citation statements)
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“…When NRN was controlled for the 1 kg mass moved far away from borderline statistically significant. While the pH of the soil increases during decomposition [40,3], we observed it to have a smaller effect compared to NRN, as assessed by PERMANOVA R 2 (25 and 50 % less on average in 16S and 18S data, respectively).…”
Section: Discussionmentioning
confidence: 53%
See 1 more Smart Citation
“…When NRN was controlled for the 1 kg mass moved far away from borderline statistically significant. While the pH of the soil increases during decomposition [40,3], we observed it to have a smaller effect compared to NRN, as assessed by PERMANOVA R 2 (25 and 50 % less on average in 16S and 18S data, respectively).…”
Section: Discussionmentioning
confidence: 53%
“…The 1 kg carcasses were marginally statistically significant compared to other masses, particularly the 50 kg mass. However, all other carcass masses (20,40, and 50 kg) did not display significant differences in their microbial communities throughout decomposition. This finding suggests that microbial clocks to estimate the postmortem interval may be robust to human cadaver mass, at least between 20-50 kg.…”
Section: Discussionmentioning
confidence: 88%
“…When corpses rupture they release an ammonia-rich, high nutrient fluid that alters both the pH and nutrient content of the soil (Meyer et al, 2013). Accordingly we saw a predictable spike in gravesoil pH from ∼6.0 to ∼8.5 (Figure 1B) and declines in Acidobacteria (Figure 2A), the abundance of which is known to be inversely related to soil pH (Lauber et al, 2009).…”
Section: Resultsmentioning
confidence: 99%
“…3). The timing of rupture coincides with a predictable increase in soil pH indicative of rupture as ammonia-rich fluids are released into the soil (24). Furthermore, the stage of decomposition was assessed with visual score data following Megyesi et al (9).…”
Section: Resultsmentioning
confidence: 99%