Late Paleocene to early Oligocene fire ecology of the south Mongolian highland

نویسندگان

چکیده

Changes in fire ecology during warm and cold periods the geological past are important because of their effects on terrestrial ecosystems global carbon cycle. We examined charcoal concentrations Erden Obo section Inner Mongolia to reconstruct evolution wildfire relationship regional vegetation from Late Paleocene through Early Oligocene. Our data show that frequency were relatively high end beginning Eocene, accord with other paleofire records worldwide. However, low occurred Eocene Climate Optimum (EECO), coincident change shrubland forest due strengthening rainfall, we suggest humid climate may have been responsible for this decrease. High after Middle near-synchronously transition steppe. The high-frequency was most likely triggered by drought aridification process Eocene. propose these temporal changes consistent within northern temperate zone Oligocene, studies wildfires need be evaluated context paleovegetation zones ecosystem evolution.

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ژورنال

عنوان ژورنال: Frontiers in Earth Science

سال: 2023

ISSN: ['2296-6463']

DOI: https://doi.org/10.3389/feart.2023.1171452