“…Preservation of fossil leaves is a multiscale process that depends on a variety of environmental inputs such as climate, the site of the preserved plant assemblage, the local environment (during burial), vicissitudes of leaf damage, the chemical milieu of the plant specimens, and other factors (Behrensmeyer et al, 2000; DiMichele & Gastaldo, 2008; Greenwood & Donovan, 1991). Moreover, the observation of DTs is dependent on a fossil plant assemblage that has achieved or exceeded a threshold in which the plant specimens are sufficiently well preserved, abundant, diverse, and unbiased, and have voucher specimens deposited in an institution accessible to other researchers (e.g., Currano et al, 2021; Gunkel & Wappler, 2015; Maccracken et al, 2022; Wilf, 2008; Xiao, Labandeira, Dilcher, & Ren, 2022a, 2022b). Developing better models that consider preservational bias, such as mode of preservation, will provide error margins for estimating interactions in a manner that is site‐ and taxon‐specific, thereby allowing for quantification of site preservation quality.…”