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species between the Permian and the end of 1. Erwin, D. Sci. Am. 275, 72–78 (1996). 7. Gastaldo, R. A., Neveling, J., Geissman, J. W. & the Middle Triassic (between 251.9 million and 2. Burgess, S. D., Bowring, S. & Shen, S. Z. Proc. Natl Kamo. S. L. Geol. Soc. Am. Bull. 130, 1411–1438 Acad. Sci. USA 111, 3316–3321 (2014). (2018). around 237 million years ago) has focused on 3. Payne, J. L. & Clapham, M. E. Annu. Rev. Earth 8. Collinson, J. W., Hammer, W. R., Askin, R. A. & the effects of a global trend towards aridifica- Planet. Sci. 40, 89–111 (2012). Elliot, D. H. Geol. Soc. Am. Bull. 118, 747–763 (2006). tion. It was proposed that, after a worldwide 4. Fielding, C. R. et al. Nature Commun. 10, 385 9. Benton, M. J. Phil. Trans. R. Soc. A 376, 20170076 collapse of plant communities and a mass (2019). (2018). 5. Nowak, H., Schneebeli-Hermann, E. & 10. Smith, R. H. M. & Botha-Brink, J. Palaeogeogr. extinction of species that cascaded through the 9 Kustatscher, E. Nature Commun. 10, 384 (2019). Palaeoclimatol. Palaeoecol. 396, 99–118 (2014). food chain , there was a change in the floral 6. Behrensmeyer, A. K., Kidwell, S. M. & Gastaldo, R. A. 11. Sues, H. D. & Fraser, N. C. Triassic Life on Land: The species across global landscapes by the Middle Paleobiology 26, 103–147 (2000). Great Transition (Columbia Univ. Press, 2010). Triassic period. For the demise of Glossopteris, Fielding and colleagues find no evidence of an aridification trend in their region that would CONDENSED-MATTER PHYSICS suggest that a hot terrestrial landscape pro- moted a mass extinction of plants during the time of the end-Permian crisis. This conclusion of Fielding and colleagues’ Materials in flatland regional work is supported by a comprehen- sive analysis of plant fossil records on a global scale conducted by Nowak and colleagues. twist and shine The authors analysed the patterns of previ- ously reported plant fossils from 259.1 mil- Four studies demonstrate the vast opportunities provided by stacking pairs of lion to around 237 million years ago, which monolayer materials and changing the resulting optical properties by twisting spans the end-Permian mass extinction and one material with respect to the other. See Letters p.66, p.71, p.76 & p.81 the Early and Middle Triassic. They gener- ated a database that includes information on more than 7,300 plant macrofossils and nearly BERNHARD URBASZEK & AJIT SRIVASTAVA be stacked on top of each other to form what is 43,000 fossil records of pollen or spores. So known as an artificial heterobilayer (Fig. 1a). far, this is the most comprehensive database tomically thin materials are currently If the layers are periodic crystals that have generated for floral analysis before and after being investigated for fundamental slightly different lattice constants, the elec- the end-Permian crisis. It amasses the evidence research and applications in optics tronic properties of each layer are modified that has been considered by many palaeontol- Aand electronics, because they interact strongly by the presence of the other layer. Specifically, ogists to indicate a trend in mass extinction with light and have fascinating magnetic the electronic states and band structure of of terrestrial plants that mirrors that of the properties. When two different monolayer the heterobilayer depend on the spacing and marine mass extinction9. materials are brought into contact to form a relative alignment of the atoms. The authors present origination, extinction bilayer, electrons can no longer move freely in Because of the slight mismatch in the and turnover patterns at the level of species and the planes of the atomic layers. Instead, they lattice constants of the two layers, arrangements genera on a stage-by-stage basis (stages being are trapped in spatially periodic potential- of atoms in the heterobilayer change periodi- steps in the geological timescale). The diver- energy variations called moiré potentials, as cally: atoms of metals (such as molybdenum sity of genera was relatively constant across the a result of interactions between the layers1. and tungsten) are positioned on top of each time interval, although the species diversity of These nanometre-scale potentials are caused other at certain points, whereas atoms of chal- macrofloral fossils dropped 251.9 million years by the layers having different orientations or cogens (such as sulfur and selenium) are aligned ago. The diversity of genera represented by lattice constants — parameters that describe at other points. These different configurations spores and pollen remained constant across the dimensions of a unit cell in a crystal of atoms, known as registries, result in differ- the time frame studied, although Nowak et al. lattice. Moiré potentials have been predicted ent energies for the valence and conduction note a small decline in species-level diversity to strongly modify the optical properties of bands, as verified by scanning tunnelling micro around 251.9 million years ago. Of the groups such bilayers2. Four papers in this issue3–6 scopy1. Consequently, electrons in the plane of of plants that have either pollen or spores, report observations of optical emission and the heterobilayer are subject to periodically the spore-bearing ferns, as well as the pollen- absorption that confirm this prediction. changing bands, and, if the variations in the producing seed ferns and cycads, declined Monolayers of materials called transition- band energies are sufficiently large, electrons in diversity during this time, whereas the metal dichalcogenides (TMDs) have strong are trapped in moiré potentials. pollen-bearing conifers and ginkgos increased in-plane covalent bonds, and can therefore An attractive feature of such heterobilayers in diversity. be produced by exfoliation (the removal of is the tunability of their periodic potential. In contrast to prevailing wisdom, Nowak sheets from a bulk crystal) in a similar way to Adding a slight twist during the stacking pro- and colleagues demonstrate that land plants graphene — a single layer of carbon atoms. cess, or exchanging one lattice with another did not experience widespread extinction However, unlike graphene, atomically thin that has a different lattice constant, leads to during Earth’s most severe biological crisis. TMD crystals are semiconductors that have moiré potentials that have a different spatial Their conclusion is similar to that drawn for an energy gap between their higher-energy periodicity. This feature enables the electronic terrestrial vertebrates11. This leaves the rela- (conduction) and lower-energy (valence) properties of layered materials to be tailored in tionship between the end-Permian marine electronic bands. Consequently, charge carri- a fundamentally new way. As a result, hetero mass extinction and the effect on land at the ers in these materials that are excited by light or bilayers are becoming a playground for explor- time enigmatic for now, and still up in the air that are injected using a voltage can relax from ing exotic quantum phenomena — rather like for further investigation. ■ the conduction band to the valence band by how the strong interactions between electrons emitting particles of light (photons). in twisted bilayers of graphene have led to the Robert A. Gastaldo is in the Department of Just as the weak attraction between layers spectacular observation of superconductivity Geology, Colby College, Waterville, Maine lends itself to exfoliation, it also allows two in electronic-transport studies7. 04901, USA. monolayers of different TMDs (such as tung- The four current papers investigate the e-mail: [email protected] sten disulfide and molybdenum diselenide) to impact of moiré potentials on light emission
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a b c
Conduction Hybridized band Electron exciton