2022
DOI: 10.1016/j.cretres.2021.105065
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Brachyoxylon fossil woods with traumatic resin canals from the Upper Cretaceous Cerro Fortaleza Formation, southern Patagonia (Santa Cruz Province, Argentina)

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Cited by 15 publications
(10 citation statements)
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“…Nevertheless, the fossil woods from the Kachaike Formation differ from B. patagonicum described by Rombola et al (2022) only in the absence of traumatic resin canals. However, these types of canals are formed as defensive responses of the plant against abiotic or biotic alterations, therefore the taxonomic relevance of this character is limited (Rombola et al, 2022).…”
Section: Remarks and Comparisonsmentioning
confidence: 75%
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“…Nevertheless, the fossil woods from the Kachaike Formation differ from B. patagonicum described by Rombola et al (2022) only in the absence of traumatic resin canals. However, these types of canals are formed as defensive responses of the plant against abiotic or biotic alterations, therefore the taxonomic relevance of this character is limited (Rombola et al, 2022).…”
Section: Remarks and Comparisonsmentioning
confidence: 75%
“…In turn, these specimens share all the characteristics (e.g., distinct growth rings, exclusively uniseriate rays, araucarioid cross-fields with up to 8 pits per field) with Brachyoxylon patagonicum Rombola, Greppi & Pujana, from the Upper Cretaceous of Argentinean Patagonia (Rombola et al, 2022). Nevertheless, the fossil woods from the Kachaike Formation differ from B. patagonicum described by Rombola et al (2022) only in the absence of traumatic resin canals. However, these types of canals are formed as defensive responses of the plant against abiotic or biotic alterations, therefore the taxonomic relevance of this character is limited (Rombola et al, 2022).…”
Section: Remarks and Comparisonsmentioning
confidence: 75%
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“…Lacovara et al [ 25 ] interpreted these deposits to represent a crevasse splay horizon deposited onto a fluvial floodplain, based on an abundance of large-scale (primary), convoluted bedforms interpreted to have formed either (1) via liquefaction during rapid deposition, or (2) by sediment redistribution around the large, heavy skeletal remains of the Dreadnoughtus holotype at the time of burial, as it subsided into a thick, “soft” substrate. Abundant silicified wood [ 41 ] and palynomorphs [ 42 ] in strata of the Cerro Fortaleza Formation demonstrate that fluvial floodplains across the region hosted diverse forests.…”
Section: Geologic and Taphonomic Contextmentioning
confidence: 99%