@Hammerwarjournals.sagepub.com/doi/10.1177/0959683613493936 : In summary, the evolution of fire history in the study profiles across the region is closely related to (1) gradients in humidity; (2) spatial and temporal variability in the distribution and intensity of human land use; and (3) www.sciencedirect.com/science/article/abs/pii/S1040618211001698 : High-resolution quartz-based SAR-OSL dating contributes to the establishment of a reliable chronological framework for the landscape evolution at two type sites for the human occupation during the Weichselian–Holocene transition in the Belgian Campine region. Both sites, Lommel-Maatheide and Arendonk-Korhaan, present a similar stratigraphy: pure sands intercalated by a bleached horizon that laterally grades into a peat layer www.semanticscholar.org/paper/Charcoal-in-soils-of-the-Allerød-Younge no se para que pongo el título: Charcoal in soils of the Allerød-Younger Dryas transition were the result of natural fires and not necessarily the effect of an extra-terrestrial impact
@parladoiro del primer articulo "The increase in fire activity occurs in the recent loess layer (L0) and the surface soil (TS) consistent with the establishment of irrigated farming for cereal cultivation in the southern part of the study region about 3100 yr BP. Broad-scale land reclamation was extended to the loess tableland region about 2170–1730 yr BP (during the Qin-Han Dynasty period)" Pero no hablábamos del Younger Dryas?
Del segundo: Sabes que la turba no viene del carbón, no? te indica sólo una acumulación de materia orgánica, y además es un cambio lateral, o sea, que es una acumulación orgánica como puedes tener en cualquier sitio.
Sobre el tercero, que ya te lo he comentado antes, el carbon no tiene porque venir de incendios antropogénicos, de hecho ese artículo te dice que son naturales, que son debidos a que tras el enfriamiento del Younger Dryas, las especies de pinos termófilas, mueren masivamente, y eso produce mucha acumulación de materia orgánica, facilmente combustible, nada más, en ningún lado dice que son antropogénicos.
@Hammerwar del primer árticulo: Effective moisture variability on century to millennial timescales and regional differences in fuel availability appear to be the most important controls on fire from the Lateglacial period to the mid Holocene (12,000–3100 yr BP). Conversely, asynchronous fire patterns during the late Holocene appear to indicate regional and temporal variations as well as changing intensities of human activity. Que se haya intensificado no significa que hace 12.000 año no fueran los causantes.
El segundo, el lugar es al lado del Usselo, es el yacimiento importante para la evolución de los asentamiento en la época antes, durante y después del estrato de Usselo, que no es de turba como ya se lleva puesto en bastantes mas entradas: maajournal.com/Issues/2010/Vol10-4/5_Derese.pdf
www.sciencedirect.com/science/article/abs/pii/S1040618211001698 : High-resolution quartz-based SAR-OSL dating contributes to the establishment of a reliable chronological framework for the landscape evolution at two type sites for the human occupation during the Weichselian–Holocene transition in the Belgian Campine region. Both sites, Lommel-Maatheide and Arendonk-Korhaan, present a similar stratigraphy: pure sands intercalated by a bleached horizon that laterally grades into a peat layer
www.semanticscholar.org/paper/Charcoal-in-soils-of-the-Allerød-Younge no se para que pongo el título: Charcoal in soils of the Allerød-Younger Dryas transition were the result of natural fires and not necessarily the effect of an extra-terrestrial impact