page_title: Fossil record of fire
section_title: Fossil evidence
hierarchical_section_title: Fossil record of fire / Fossil evidence
context_page_description: The fossil record of fire first appears with the establishment of a land-based flora in the Middle Ordovician period, 470 million years ago, permitting the accumulation of oxygen in the atmosphere as never before, as the new hordes of land plants pumped it out as a waste product. When this concentration rose above 13%, it permitted the possibility of wildfire. Wildfire is first recorded in the Late Silurian fossil record, 420 million years ago, by fossils of charcoalified plants. Apart from a controversial gap in the Late Devonian, charcoal is present ever since. The level of atmospheric oxygen is closely related to the prevalence of charcoal: clearly oxygen is the key factor in the abundance of wildfire. Fire also became more abundant when grasses radiated and became the dominant component of many ecosystems, around 6 to 7 million years ago; this kindling provided tinder which allowed for the more rapid spread of fire. These widespread fires may have initiated a positive feedback process, whereby they produced a warmer, drier climate more conducive to fire.
context_section_description: The fossil evidence of fire comes mainly from charcoal.  The earliest charcoal dates to the Silurian period. Charcoal results from organic matter exposed to high temperatures, which drives off volatile elements and leaves a carbon residue. Charcoal differs from coal, which is the fossilised remains of living plants and burns to leave soot.
  Fossil charcoal is known as fusain, a crumbly silky material which may form blocks or microscopic films. Plants can be preserved in exquisite detail, and original cell structures can often be preserved in three dimensions. Spectacular images can be recovered using scanning electron microscopy.  Fragments can be distributed some distance, and soot-rich layers in strata deposited by deltas can provide a 'time-averaged' record of fire activity in the catchment (and up-wind) area of the river.
  The loss of volatile elements during combustion means that charred remnants are usually smaller than the original organism, but this same factor makes them unlikely to be eaten by any animals (for they have no nutritional value), enhancing their preservation potential.
  Evidence of lightning strikes is usually difficult to link to specific fires; occasionally they may scorch trees, but fulgarites - fused sediments where soil has been melted together by a strike - are occasionally preserved in the geological record from the Permian onwards.
  Scorched layers of trees which survived fires can also provide evidence of fire frequency - especially as they can be related to the annual growth rings of the affected tree.  These are useful for relatively recent times, but there are only putative reports of this phenomenon in pre-Tertiary strata.
caption: Modern charcoal
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