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. 2020 May 14;8:e9139. doi: 10.7717/peerj.9139

Table 1. Age, locality, size, and diversity of studied samples from the Cassian Formation.

Samples from Lago Antorno, Misurina landslide, Settsass, and Stuores are from previous studies (Hausmann et al., 2019, unpublished data; Nützel & Kaim, 2014; Hausmann & Nützel, 2015). See ‘Methods’ for applied measures. Indices based on 10 most abundant species per sample. PPD = pairwise proportional dissimilarity. Mean PPD with regard to other samples. Inferred relative water depth is based on ranking detailed in Table S1: Positive values refer to deeper settings, negative values to shallower settings.

Locality Stratigraphic age (ammonite biozone, substage) Coordinates Reference No. of specimens Berger-Parker dominance index Evenness Mean PPD Inferred relative water depth rank
Costalaresc austriacum, Julian 46.53995N 12.16390E This study 315 0.73 0.29 0.91 ± 0.04 −1
Lago Antorno probably austriacum, Julian 46.59438N 12.26100E Hausmann et al. (2019, unpublished data) 216 0.31 0.50 0.88 ± 0.06 −4.5
Misurina landslide probably austriacum, Julian 46.59490N 12.25962E Hausmann et al. (2019, unpublished data) 558 0.30 0.48 0.89 ± 0.06 −2
Picolbach aon, Julian 46.53427N 11.92253E This study 213 0.28 0.54 0.92 ± 0.04 4
Rumerlo cliff probably aonoides, Julian 46.53375N 12.09882E This study 229 0.22 0.54 0.91 ± 0.04 −4
Rumerlo ski slope aonoides, Julian 46.53684N 12.10214E This study 33 0.21 0.58 0.93 ± 0.05 −5
Settsass aon, ”Cordevolian” 46.51733N 11.95846E Nützel & Kaim (2014) 296 0.24 0.50 0.91 ± 0.04 2
Stuores aon, ”Cordevolian” 46.52872 N 11.93672E Hausmann & Nützel (2015) 1026 0.33 0.53 0.95 ± 0.02 −6