Pseudopanax ferox ( Kirk, 1889 )

Pole, Mike, 2022, A vanished ecosystem: Sophora microphylla (Kōwhai) dominated forest recorded in mid-late Holocene rock shelters in Central Otago, New Zealand, Palaeontologia Electronica (a 1) 25 (1), pp. 1-41 : 22

publication ID

https://doi.org/ 10.26879/1169

DOI

https://doi.org/10.5281/zenodo.10997960

persistent identifier

https://treatment.plazi.org/id/0D07EA56-FF8E-FFB4-FEF4-FC2F56B9FF65

treatment provided by

Felipe

scientific name

Pseudopanax ferox ( Kirk, 1889 )
status

 

Pseudopanax ferox ( Kirk, 1889) View in CoL

Figure 22 View FIGURE 22

Material. Present in 4% of the shelters with dry vegetation. Shelter-001: LX2711, LX2712; Shelter-037: LX3111; Shelter-066: SL 6467; Shelter-094: LX2884.

Remarks. An intact Pseudopanax ferox leaf was found at Gibraltar Rock and Sbag 0870 (LX3111, ConcJar 2204). This, and cuticle fragments from other shelters, show the ring of subsidiary cells, and prominent outer stomatal ledges which are surrounded by a ring of thin, finely ridged cuticle, which is typical of Pseudopanax . This specimen also shows the normal epidermal cells which are much smaller than the stomatal complexes, and tangentially oriented subsidiary cells, which distinguish P. ferox from Pseudopanax crassifolious Koch (1859) . The later has much larger normal epidermal cells, and larger, more irregularly shaped subsidiary cells. P. ferox is considered to have existed in mid-late Holocene Central Otago ( Walker et al., 2004b; Rogers et al., 2005), but to date, not P. crassifolious . However, a single relict specimen of P. crassifolious is living in the Waikerikeri Valley (pers. obs.), indicating both species were likely in the region, and recognising the difference is important.

SL

University of Sierra Leone, Njala University College

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