Orthion veracruzense
Accumulation profile
- Substrate
- Ni-bearing volcanic-ash soils (non-ultramafic)
- Habitat
- Lowland evergreen rainforest
- Distribution
- Mexico (Veracruz, Los Tuxtlas; also Chiapas)
- First reported
- 2024 · Navarrete Gutiérrez et al.
- Verification
- primary-measured
Description & ecology
Field-collected leaves (HNO₃–H₂O₂ digest, ICP) ranged 815–4,290 µg g⁻¹ Ni (mean 2,520 ± 1,490, N=5; Navarrete Gutiérrez et al. 2024, Ecological Research 39:879–893, doi:10.1111/1440-1703.12504): 'Foliar samples of O. veracruzense had a minimum Ni concentration of 815 mg kg−1 and a maximum of 4290 mg kg−1 (mean of 2520 mg kg−1)'.
Facultative: only 12% of 89 herbarium specimens exceeded the 1,000 µg g⁻¹ threshold.
Notable as a Ni hyperaccumulator from basaltic volcanic soils rather than ultramafic serpentinite.
References
- Reeves, R. D., Baker, A. J. M., Jaffré, T., Erskine, P. D., Echevarria, G., & van der Ent, A. (2018). A global database for plants that hyperaccumulate metal and metalloid trace elements. New Phytologist, 218, 407–411. doi:10.1111/nph.14907