ABSTRACT:The relief of the regions of Manaus and Itacoatiara, Central Amazon, is supported by Neogene siliciclastic rocks, bounded at the base and top by lateritic paleosols and covered by quaternary sedimentary deposits from the Solimões-Amazon river system. This unit is informally assigned to the Novo Remanso Formation, consists of usually reddish and ferruginized sandstones, conglomerates and pelites, with few identified fossil records, a fact that has hindered its stratigraphic position, and the paleoenvironmental reconstruction of the last phase of the Amazon Basin settling. This study describes, for the first time, the occurrence of fossil wood in outcroppings of the left bank of the Amazon River, where anatomical and morphological data has enabled its characterization to the species level. Thus, the data marks the record of the Annonaceae in South America, as well as the depositional processes related to incorporation of organic material in the sandy layer and the fossilization processes that allowed its preservation. In an unprecedented way, this study has described Duguetiaxylon amazonicum nov. gen and sp. and provided information on the anatomical and systematic character, as well as data on plant-insect interaction, and a better understanding of the family.
KEYWORDS:Annonaceae; Duguetiaxylon; Neogene Deposit; Amazon Basin.
RESUMO: O relevo das regiões de Manaus e Itacoatiara, na Amazônia Central, é suportado por rochas siliciclásticas neogênicas, delimitadas na base e no topo por paleossolos lateríticos e cobertas por depósitos sedimentares quaternários do sistema fluvial Solimões-Amazonas. Essa unidade é informalmente atribuída à Formação Novo