Journal of Biogeography SUPPORTING INFORMATION NON CONGRUENT FOSSIL AND PHYLOGENETIC EVIDENCE ON THE EVOLUTION OF CLIMATIC NICHE IN THE GONDWANA GENUS NOTHOFAGUS Luis Felipe Hinojosa, Aurora Gaxiola, María Fernanda Pérez, Francy Carvajal, María Francisca Campano, Mirta Quattrocchio, Harufumi Nishida, Kazuhiko Uemura, Atsushi Yabe, Ramiro Bustamante and Mary T. K. Arroyo Appendix S1: Systematic Descriptions of the fossils Description of leaf remains associated with Nothofagus from Ligorio Marquez Formation. Leaf remains were described using the terminology following to Hickey (1973) and Ellis et al. (2009). Nothofagus subferruginea (Dusén) Tanai (Fig. S1) Fagus ferruginea Dusén, 1899, Svenska Expeditionen till Magellansländerna. Bd. I, No. 4: p. 94, Taf. 8, figs. 1-8. Nothofagus subferruginea (Dusén) Tanai, 1986, Jour. Fac. Sci., Hokkaido Univ., ser. 4, 21(4): p. 531, pl. 9, figs. 1-12; pl. 11, figs. 3-5; Text-figs. 7D-F. Description: Lamina symmetrical, microphyll, elliptic to narrow elliptic or ovate; apex acute, straight on both sides; base nearly right angle, convex; length 2.6 to 70 mm; width 11 to 31 mm; length to width ratio 2.3 to 3.1; petiole marginal, up to 7.3 mm long; margin compound. Teeth concave-concave or concave-flexuous with rounded sinuses; regularly spaced; tooth apex acute, apically oriented, secondary vein enters primary and secondary tooth medially or slightly basally. Venation pinnate; primary vein moderate, straight; secondaries craspedodromous, moderate, up to fourteen pairs, regularly spaced, arising at an acute angle on the middle portion, straight, decurrent at divergence on the basal part, abruptly bend up within the marginal teeth; tertiaries thin, L.F. Hinojosa et al. Climatic Niche in Nothofagus 1 eight to ten per 1 cm, mixture of alternate and opposite percurrent, obtuse to the midvein; quaternary veins moderate, orthogonal, forming moderately-developed areolations; areoles four- or more-sided, medium; veinlets very thin, branching several times. Discussion: Five specimens were obtained from the Ligorio Márquez Formation. These are characterized by pinnate secondaries with compound marginal teeth, in which secondary veins enter tooth apex directly. General morphological characteristics of this species are comparable with leaves assigned to Nothofagus described from the late Paleogene to Miocene of South America and Antarctic Peninsula. Among Fagus and Nothofagus leaves described so far, our materials are most similar to Fagus subferruginea Dusén that was originally described from the Loreto Formation near Punta Arenas in Chile and Formation at Barranca de Carmen Sylva in Fuego Island, Argentina. After detailed examination of additional materials from the same formation with the lectotype, Tanai (1986) transferred this species to the genus Nothofagus, based on craspedodromous secondaries and branched veinlets, which we would support in this manuscript. Materials: NSM PP-12344-12348. Occurrence: Loc. LMZ-2 (NSM PP-12345-12348), LMZ-7 (NSM PP-12344), Ligorio Márquez Formation L.F. Hinojosa et al. Climatic Niche in Nothofagus 2 Figure S1 Nothofagus subferruginea (Dusén) Tanai. Photographs 1, 2, 6 NSM PP12345; Photographs 3 & 6 NSM PP-12346; Photograph 4 & 9 NSM PP-12348; Photographs 5 & 7 NSM PP-12344; Photographs 1,2,3,5 Natural size; Photograph 3 x 1.5. L.F. Hinojosa et al. Climatic Niche in Nothofagus 3 Nothofagus serrulata Dusen (Fig. S2) Nothofagus serrulata Dusen 1907 Uber die tertiare Flora der Magellanslander I.- In: Nordenskjold, O (ed.): Wiss. ErgebSchwed. Exp. Magellanslandern. 1895-98 IV: 84108-Stockholm. Description: Lamina symmetrical, microphyll, ovate; apex acute, short acuminate; base obtuse, convex; 3.95- 4.5 cm length and 2.10-2.5 cm width; length to width ratio 1.81.88; petiole marginal, ca. 5 mm long; margin compound. Marginal teeth irregularly spaced, 7 teeth per 1 cm; primary teeth straight/convex, apically oriented; secondary teeth convex/retroflex in shape exmedially oriented; tooth apex acute with blunt tip; sinus acute; secondary vein enters primary and secondary tooth slightly basally. Venation pinnate; primary vein stout, straight, slightly sinuous near the apical one-third the lamina; secondary veins craspedodromous, moderate, fourteen pairs, regularly spaced, arising at narrow acute to acute angle on the middle portion, straight, basal few pairs decurrent at divergence, abruptly bend up within the marginal teeth; tertiaries thin, 12 veins per 1 cm, sinuous, alternate percurrent, obtuse to the midvein; quaternary veins relatively thick, polygonal reticulate; areoles irregular, moderately developed; veinlets very thin, up to twice branching. Discussion: The specimen was identical to the genus Nothofagus in its venation pattern; craspedodromous secondary veins and moderately developed areoles sided by third and fourth order venation bearing branching veinlets. It is easily distinguished from the above-described N. subferruginea (Dusén) Tanai by characteristic marginal teeth, sinus as well as vein thickness. The fossils descriptions agree with the previously described Nothofagus serrulata Dusen 1907 from Barranca de Carmen Silva and around Punta Arenas Chile, Loreto Formation. N. serrulata was associated with the modern taxa N. L.F. Hinojosa et al. Climatic Niche in Nothofagus 4 alessandrii (Romero & Dibbern 1958). However, and accordance with teeth characters, numbers of secondary veins, pattern in third and fourth order venation, it is possible to associate with the modern subgenus Lophozonia, close to the modern relative N. obliqua. Other localities: Rio Chico, west of Estacion San Sebastian, Fuego Island, Chile; Brush Lake Formation, Early Miocene and Rio Turbio, Santa Cruz, Argentina)(Romero & Dibbern 1985, Tanai 1981). Materials: NSM PP-12349. SGO 1571 Occurrence: Loc. LMZ-2, Ligorio Márquez Formation. Figure S2 Nothofagus serrulata Dusen. Photographs 1 to 3 NSM-PP-12349. L.F. Hinojosa et al. Climatic Niche in Nothofagus 5 Systematics descriptions of Nothofagus pollen fossils. Nothofagidites dorotensis Romero 1973 Diagnosis: Scabrastephanocolpate, mid sized 29 μm, intectate 0.5 – 0.6 μm, colpi costate, scabrae < 1 μm, distributed densely over the entire grain. Specimens: LMF024 W23/4; LMF020 G43 1-2; LMF052 G11. Description: Monad, radial, isopolar, amb polygonal; stephanocolpate, 6 colpi, colpi costate, 12 μm long, 3 μm wide, costae 0.3 – 0.5 μm; intectate, nexine 0.5 μm thick; sculpture scabrate, scabrae < 1 μm, 1 – 2 μm apart, distributed densely over entire grain. Dimensions: Equatorial diameter lenght 25(29)40 μm, (I/E)= colpi length/equatorial diameter lenght 0.34(0.4 )0.52 μm, nm: 26; no: 46. Botanical affinity: Nothofagaceae family Distribution: Ligorio Marquez Formation (Early Eocene; Carvajal, 2013). Colorado Basin (Neogene) well Cx-1 (Guler et al., 2001). Ñirihuau Basin (Late Eocene/Early Oligocene), Salto del Macho Formation; (Early Oligocene/Miocene?) Río Foyel Formation (Barreda et al., 2003; Cornou et al., 2012). Golfo San Jorge Basin (Danian), Cerro Bororó Formation (Volkheimer et al., 2007); (Early Miocene) Chenque Formation (Barreda, 1989; 1996; Barreda 1997a). Austral Basin (Maastrichtian/Paleocene) Cerro Dorotea Formation (Romero, 1973); (Eocene), Río Turbio Formation (Romero, 1977); (Late Eocene/Early? Oligocene); (Late Oligocene) Río Leona Formation (Barreda et al., 2009); (Oligocene) San Julián Formation (Barreda, 1997b; Náñez et al., 2009); (Late Oligocene/Early Miocene) Well Aries x-1 (Palamarczuk y Barreda, 2000). Cordillera Fueguina (Late Eocene/Early? Oligocene) Sloggett Formation (Olivero et al., 1998); Estancia La Correntina (Rosello et al., 2004). Chile: Osorno-Llanquihue Basin (Eocene) Cheuquemó Formation (Troncoso & Barrera, 1980). L.F. Hinojosa et al. Climatic Niche in Nothofagus 6 Nothofagidites acromegacanthus Menéndez y Caccavari 1975 Diagnosis: Scabrastephanocolpate, intectate <0.5 μm, colpi costate, scabrae < 0.5 μm distributed in the equator area and scabrae 0.5 – 1 um distributed densely in the polar area. Specimens: LMF021 R39 3; LMF052 R13 3: LMF024 D45; LMF024 Q35 Description: Monad, radial, isopolar, amb polygonal; stephanocolpate, 6 colpi, colpi costate, 8 - 10 μm long, 3.5 - 4 μm wide, costae 0.7 - 1 μm; intectate, nexine 0.5 μm thick; sculpture scabrate, scabrae < 0.5 μm distributed in mesocolpi and scabrae 0.5 – 1 um distributed densely in apocolpi. Dimensions: Equatorial diameter lenght 21 (24.7) 30 μm, (I/E)= colpi length/equatorial diameter lenght 0.25 (0.37 ) 0.44 μm, nm: 7 ; no: 9 Botanical affinity: Nothofagaceae family Distribution: Ligorio Marquez Formation (Early Eocene; Carvajal, 2013). Ñirihuau basin (Late Eocene/Early Oligocene), Salto del Macho Formation (Cornou et al., 2012); (Early Oligocene /Miocene?) Río Foyel Formation (Barreda et al., 2003). Golfo San Jorge Basin (Early Miocene) Chenque Formation (Barreda, 1989, 1996, 1997a); (Late Oligocene/Miocene) Golfo San Jorge (Barreda & Palamarczuk, 2000b). Austral Basin (Eocene), Río Turbio Formation (Archangelsky & Romero, 1974; Romero, 1977); (Late Oligocene) Río Leona Formation (Barreda et al., 2009); (Late Oligocene/Early Miocene); (Late Oligocene) San Julián Formation (Upper section) (Barreda, 1997b); Well Aries x-1 (Palamarczuk & Barreda, 2000). Cordillera Fueguina (Late Eocene/Early? Oligocene) Sloggett Formation (Olivero et al., 1998). Chile: OsornoLlanquihue Basin (Eocene) Cheuquemó Formation (Troncoso & Barrera, 1980). Antarctica (Campanian-Danian) López de Bertodano Formation and (Paleocene) Sobral Formation (Baldoni & Barreda, 1986). L.F. Hinojosa et al. Climatic Niche in Nothofagus 7 Nothofagidites kaitangataensis (Te Punga) Romero 1973 Diagnosis: Scabrastephanocolpate, mid sized 29.5 μm, intectate, colpi costate with Ushaped, scabrae < 0.5 μm, distributed densely over the entire grain. Specimens: LMF020 Q23 4 (2); LMF020 G12 1; LMF021 T12 1 Description: Monad, radial, isopolar, amb polygonal; stephanocolpate, 7-8 colpi, colpi costate, 10 μm long, 3 μm wide, with U-shaped, costae 1 μm; intectate, nexine 0.7 μm thick; sculpture scabrate, scabrae < 0.5 μm, distributed densely over the entire grain. Dimensions: Equatorial diameter length 27(29.5) 31 μm, (I/E)= colpi length/equatorial diameter length 0.32 (0.33) 0.35 μm, nm: 6; no: 23. Botanical affinity: Nothofagaceae family Distribution: Ligorio Marquez Formation (Early Eocene; Carvajal, 2013). In South America this group is represented by one single morphospecie: N. kaitangataensis (Te Punga, Romero, 1973), recorded from Maastrichtian to Middle Eocene, between Punta Arenas and Tierra del Fuego (Romero & Zamaloa, 1997), it is also present in New Zealand and Australia (Dettmann et al., 1990). Nothofagus Fusca group In general the pollen of Fusca group presents amb circular, short and strongly thickened colpi with ends rounded (Romero & Zamaloa, 1997). The material belonging to this group in Ligorio Márquez is slightly degraded and the details of morphology are not clear. For this reason it was not possible to classify the grains in Fusca group (a) or (b). Specimens: LMF020 W32 4; LMF051 O7 1. L.F. Hinojosa et al. Climatic Niche in Nothofagus 8 Dimensions: Equatorial diameter length 30 μm, (I/E)= colpi length/equatorial diameter lenght 0.33 μm, nm: 2; no: 3. Botanical affinity: Nothofagaceae family References Archangelsky, S. & Romero, E.J. 1974. Polen de gimnospermas (Coníferas) del Cretácico Superior y Paleoceno de Patagonia. Ameghiniana 11, 217–248. Baldoni, A. & Barreda, V. 1986. Estudio palinológico de las Formaciones López de Bertodano y Sobral, Isla Vicecomodoro Marambio, Antártida. Paleobotánica e Palinología na America do Sul. Boletim Instituto de Geociencias. Universidade de Sao Paulo. Brasil. Serie Científica 17, 89-98. Barreda, V.D. 1989. Palinología estratigráfica de las sedimentitas terciarias del “Patagoniano” en los alrededores de Comodoro Rivadavia, Chubut y Santa Cruz. Tesis doctoral, Universidad de Buenos Aires. Barreda, V.D. 1996. Bioestratigrafia de pollen y esporas de la Formacion Chenque, Oligoceno tardio?–Mioceno de las provincias de Chebut y Santa Cruz, Patagonia, Argentina. Ameghiniana 33, 35–56. Barreda, V.D. 1997a. Palynomorph assemblage of the Chenque Formation, Late Oligocene?–Miocene from Golfo San Jorge Basin, Patagonia, Argentina: Part 3. Polycolpate and tricolporate pollen. 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Paleoclima y diversidad en la palinoflora de la Formación Ligorio Márquez. Tesis de Maestría en Ciencias Biológicas. Universidad de Chile. Cornou, M.E. 2012. Palinoestratigrafía y Palinofacies del Eoceno Medio – Oligoceno en la parte Central de la Cuenca de Ñirihuau, Argentina. Tesis Doctoral en Geología. Universidad Nacional del Sur. Dettmann, M.E. & Pocknall, D.T. 1990. Nothofagidites Erdtman ex PotonieĢ, 1960; a catalogue of species with notes on the palaeogeographic distributions of Nothofagus Bl. (southern beech). New Zealand Geological Survey, Palaeontological Bulletin, 60,1-79. Dusen, P., 1899, Svenska Expeditionen till Magellansländerna. Bd. I, No. 4: p. 94, Taf. 8, figs. 1-8. Dusen, P., 1907. Uber die tertiare Flora der Magellanslander I.- In: Nordenskjold, O (ed.): Wiss. ErgebSchwed. Exp. Magellanslandern. 1895-98 IV: 84-108-Stockholm. Ellis, B., Daly, D., Hickey, LJ., Johnson, KR., Mitchell, J., Wilf, P. & Wing, S. 2009. Manual of leaf Architecture. Cornell University Press. 67 pp. Guler, M.V., Guerstein, G.R. & Quattrocchio, M.E. 2001. Palinología del Neógeno de la perforación Cx-1, Cuenca del Colorado, Argentina. Revista Española de Micropaleontología 33, 183–204. Hickey, L. 1973. Classification of the architecture of dicotyledonous leaves. American Journal of Botany 60, 17-33. Menéndez, C.A. & Caccavari de Filice M. 1975. Las especies de Nothofagidites (polen fósil de Nothofagus) de sedimentos terciarios y cretácicos de Estancia La Sara, norte de Tierra del Fuego, Argentina. Ameghiniana 12, 165-183. Náñez, C., Quattrocchio, M. & Ruiz, L. 2009. Palinología y micropaleontología de las Formaciones San Julián y Monte León (Oligoceno – Mioceno temprano) en el subsuelo de cabo Curioso, provincia de Santa Cruz, Argentina. Ameghiniana 46, 669–693. Olivero, E.B., Barreda, V., Marenssi, S.A., Santillana, S.N. & Martinioni, D.R. 1998. Estragrafía, sedimentologia y palinología de la Formacion Slogget (Paleogeno continental), Tierra del Fuego. Revista de la Asociacion Geologica Argentina 53, 504– 516. Palamarczuk, S. & Barreda, V. 2000. Palinología del Paleogeno tardío-Neógeno temprano, pozo Aries x-1, plataforma continental Argentina, Tierra del Fuego. Ameghiniana 37, 221–234. Romero, E., 1973. Polen fósil de "Nothofagus" ("Nothofagidites") del Cretácico y Paleoceno de Patagonia. Revista del Museo de La Plata (Nueva Serie) 7, 291-303. L.F. Hinojosa et al. Climatic Niche in Nothofagus 10 Romero, J. E., 1977. Polen de gimnospermas y fagáceas de la Formación Río Turbio (Eoceno), Santa Cruz, Argentina. Centro de Investigaciones en Recursos Geológicos (CIRGEO). Unidad de Paleobotánica y Palinología : 1- 219. Romero, E. & Dibbern, M. 1985. A review of the species described as Fagus and Nothofagus by Dusen. Palaeontographica B. 187, 123-137. Romero, E.J. & Zamaloa, M.C., 1997: A key for the identification of the species and an update of the record of Nothofagidites from South America. Ameghiniana 34, 207-214. Rosello, E.A., Ottone, E.G., Haring, C.E. & Nevistic V.A. 2004. Significado tectónico y paleoambiental de los niveles carbonosos paleógenos de Estancia La Correntina, Andes Fueguinos. Revista de la Asociación Geológica Argentina, 59, 778–784. Tanai, T. 1981. Geological Notes on the Fossil Localities. In: Nishida M (ed.). A Report of the Paleobotanical Survey to Southern Chile. Chiba University, Chiba, 10-30. Tanai, T 1986. Phytogeographic and phylogenetic history of the genus Nothofagus BL. (Fagaceae) in the southern hemisphere. Journal of the Faculty of Science, Hokkaido University, Series IV. 21, 505-582. Troncoso, A. & Barrera, E., 1980. Polen del Eoceno de Osorno. Boletín Museo Nacional de Historia Natural, Chile. 37:179-203.Turner, J.C.M., 1965. Estratigrafía de Aluminé y adyacencias (provincia de Neuquén). Revista de la Asociación Geológica Argentina, 20: 153-184. Volkheimer, W., Scafati, L. & Melendi, D.L. 2007. Palynology of a Danian warm climatic wetland in central northern Patagonia, Argentina. Revista Española de Micropaleontología 39, 117-134. L.F. Hinojosa et al. Climatic Niche in Nothofagus 11 Appendix S2 Fossil pollen assemblage and weighted mean values of bioclimatic variables. Figure S1. Pollen fossils of the 11 families considered in the palaeoclimatic estimations using coexistence approach and ecological niche model. (a) Dilwynites turbeculatus Harris 1965; (b) Mauritiidites franciscoi var. minutus Van der Hammen & García 1966; (c) Bombacadites sp.; (d) Tricolpites cf. reticulate Cookson 1947; (e) Liliacidites variegatus Couper 1953; (f) Gothanipollis perplexus Pocknall & Midenhall 1984; (g) Malvacipollis diversus Harris 1965; (h) Nothofagidites kaitangataensis (Te Punga) Romero 1973; i) Diporites aspis Pocknall & Mildenhall 1984; (j) Phylocladidites mawsonii (Cookson 1947) ex Couper 1953 , and (k) Proteacidites cf. subscabratus Couper 1960. Black bars = 10 µm. (a) Araucariaceae (b) Arecaceae (c) Bombacaceae (d) Gunneraceae (e) Liliaceae (f) Loranthaceae (g) Malvaceae (h) Nothofagaceae (i) Onagraceae (j) Podocarpaceae (k) Proteaceae L.F. Hinojosa et al. Climatic Niche in Nothofagus 12 Table S1. Weighted mean values (w Mean; and 20th-80th percentile) of 19 bioclimatic variables from profiles of niche occupancy in 11 families recognized in the pollen record of Ligorio Marquez Formation used in the Coexistence Approach analysis Bombacaceae Gunneraceae w Mean Araucariaceae 15.4 (8.8-23.3) Arecaceae Bio1 23.9 (22.1-25.8) 23.7 (20.9-25.8) 15.3 (7.5-22.1) Bio2 w Mean 10.4( 7.97-12.5) 9.6( 8.4-10.4) 10.8( 8.8-12.5) 10.6( 8-12.5) Bio3 w Mean 5.1( 3.134-7.08) 8.2( 7.44-8.88) 7.1( 6-8.163) 6.6( 4.751-8.342) Bio4 w Mean 467.3( 98.8-745.7) 57( 6.4-98.8) 147.1( 52.6-191.2) 194.8( 52.6-329.8) Bio5 w Mean 27.5( 21.9-31.3) 30( 27.8-32.5) 31.6( 29-33.6) 23.8( 291-17.2) Bio6 w Mean 3.7( -5.9-14.1) 18.2( 15.8-20.8) 15.7( 10.8-19.1) 7.2( -0.9-15.8) Bio7 w Mean 11.8( 9.4-12.26) 16( 10.8-19) 16.6( 10.8-20.4) 17.4( 10.8-21.8) Bio8 w Mean 17.4( 8.2-24.3) 23.5( 21.6-25.6) 24.3( 21.6-25.6) 15.1( 6.9-22.9) Bio9 w Mean 13.4( 4.7-22.4) 24( 20.6-25.9) 22.6( 18.81-25.9) 15.2( 8.2-20.6) Bio10 w Mean 21.1( 15.3-25.7) 24.5( 22.6-26.8) 25.4( 22.6-26.8) 17.7( 11.2-23.7) Bio11 w Mean 9.2( -0.3-19.2) 23.1( 20.81-25.7) 21.7( 19.2-25.7) 12.7( 2.9-20.8) Bio12 w Mean 1310.1( 431.7-1942.7) 2793.4( 1942.7-3237.8) 1772.5( 863.4-2374.4) 1660.7( 647.6-2374.4) Bio13 w Mean 189.2( 49.7-298.4) 383.5( 248.7-447.6) 285.2( 149.2-348.1) 229.3( 99.5-298.4) Bio14 w Mean 50.4( 0-85.3) 95( 28.4-128) 43.9( 0-71.1) 64.2( 14.2-99.6) Bio15 w Mean 47( 16.2-70.3) 438( 273-54.1) 63.3( 32.4-86.5) 44.6( 16.2-70.3) Bio16 w Mean 511.5( 134.4-672) 1047( 672-1209.7) 762.7( 403.2-940.9) 625.3( 268.8-806.4) Bio17 w Mean 174( 0-236.6) 343.8( 142-473.3) 160.4( 0-284) 223.8( 47.3-331.3) Bio18 w Mean 374.3( 102.9-617.1) 541.6( 205.7-720) 431.8( 205.7-617.1) 420.6( 102.9-617.1) Bio19 w Mean 265.5( 0-373.9) 858.3( 373.9-1121.6) 367.3( 0-654.3) 375.8( 0-654.3) Liliaceae Loranthaceae Malvaceae Nothofagaceae Bio1 w Mean 9.1 (1.4-16) 21.8 (17.2-25.8) 21.6 (17.2-25.8) 14.1 (7.5-20.9) Bio2 w Mean 10.6( 8-12.5) 11.8( 9.22-14.2) 12.1( 9.6-14.2) 9.9( 7.5-11.3) Bio3 w Mean 3.8( 2.595-4.751) 6.31( 4.751-7.624) 6.2( 4.751-7.444) 5.8( 4.57-7.98) Bio4 w Mean 646.9( 376.-884.3) 260.2( 52.6-468.4) 278.5( 52.6-468.4) 284.8( 52.6-422.2) Bio5 w Mean 24.1( 17.2-30.1) 31.6( 27.8-34.8) 31.77( 27.8-34.8) 23.6( 17.2-29) Bio6 w Mean 4.7(-15.9-4.1) 11.7( 4.1-19.1) 11( 4.1-17.5) 5.6( -2.5-14.1) Bio7 w Mean 17.9( 12.2-21.8) 19.8( 12.2-27.2) 20.6( 12.2-27.2) 21.6( 16.3-25.9) Bio8 w Mean 11.8( 4.2-18.9) 23( 20.2-26.9) 22.9( 18.9-26.9) 13.4( 4.2-21.6) Bio9 w Mean 7.7( -4.1-20.6) 20.1( 13.5-24.1) 19.8( 13.5-24.1) 14.5( 8.2-20.6) Bio10 w Mean 17.3( 11.2-22.6) 24.9( 21.6-27.8) 24.8( 21.6-27.8) 17.6( 12.2-25.7) Bio11 w Mean 0.8( -10-9.4) 18.3( 11.1-24) 17.8( 11.1-24) 10.4( 1.3-19.2) Bio12 w Mean 867.9( 215.9-1079.3) 1319( 431.7-1942.7) 1184.5( 215.9-1726.9) 1658.5( 647.6-2374.4) Bio13 w Mean 129.9( 49.7-149.2) 216.7( 49.7-298.4) 197.3( 49.7-298.4) 207.5( 99.5-298.4) Bio14 w Mean 30( 0-42.7) 33.6( 0-56.9) 29.57( 0-42.7) 79.9( 28.4-113.8) Bio15 w Mean 46.25( 21.6-70.3) 62.7( 32.4-91.9) 65.5( 32.4-91.9) 32.2( 10.8-48.7) Bio16 w Mean 349.8( 134.4-403.2) 577.9( 134.4-806.4) 524.9( 134.4-806.4) 574.2( 268.8-806.4) Bio17 w Mean 106.5( 0-142) 122.1( 0-189.3) 107.4( 0-189.3) 271.9( 94.7-378.6) Bio18 w Mean 227.4( 0-308.6) 349.1( 102.9-514.3) 325.6( 0-514.3) 411.3( 102.9-617.1) Bio19 w Mean 197.5( 93.5-280.4) 250.1( 0-467.3) 206.3( 0-373.9) 415.2( 93.5-654.3) Onagraceae Podocarpaceae Proteaceae Bio1 w Mean 12.6 (5.1-22.1) 19.7 (13.6-24.6) 20.6 (16-24.5) Bio2 w Mean 9.4( 6.7-11.3) 10.5( 8.4-12.5) 13( 10.9-14.63) Bio3 w Mean 4.56( 2.775-6.546) 6.5( 4.93-8.16) 5.2( 4.571-5.648) Bio4 w Mean 477.8( 145-699.5) 226.9( 52.6-376) 421.3( 237.4-560.8) Bio5 w Mean 24.6( 18.4-31.3) 28.3( 24.3-31.3) 32.9( 29-37.2) Bio6 w Mean 1.5( -7.5-12.5) 10.9( 2.5-19.1) 7.6( 2.5-10.8) Bio7 w Mean 23( 14.9-28.6) 23.7( 13.5-31.4) 25.1( 19-30) Bio8 w Mean 14( 4.2-24.3) 20.5( 14.9-25.6) 23.1( 17.6-28.3) Bio9 w Mean 11.3( 1.2-22.4) 18.5( 11.8-24.1) 17.7( 11.8-22.4) Bio10 w Mean 18.6( 12.2-25.7) 22.4( 18.5-25.7) 25.6( 21.6-28.9) Bio11 w Mean 6.4( -3.5-19.2) 16.6( 7.8-24) 14.9( 9.4-19.2) Bio12 w Mean 1197( 431.7-1511) 1709.7( 863.4-2374.4) 792.7( 215.9-1079.3) Bio13 w Mean 172.1( 49.7-248.7) 257.8( 149.2-348.1) 145.6( 49.7-198.9) Bio14 w Mean 45( 0-71.1) 56.2( 0-99.6) 17.7( 0-28.4) Bio15 w Mean 41.8( 16.2-64.9) 53.7( 21.6-81.1) 63.2( 27-91.9) Bio16 w Mean 465.2( 134.4-6723) 696.3( 268.8-940.9) 383.9( 0-537.6) Bio17 w Mean 156( 47.3-236.6) 197.5( 0-331.3) 66.2( 0-94.7) Bio18 w Mean 285.4( 102.9-411.4) 477.4( 205.7-617.1) 281.2( 0-411.4) Bio19 w Mean 287.2( 0-373.9) 335.9( 0-560.8) 97.9( 0-93.5) L.F. Hinojosa et al. Climatic Niche in Nothofagus 13 Table S2. Weighted mean values of 13 bioclimatic variables from profiles of niche occupancy in Nothofagus. Loc: Modern distribution; SA: South America; NZ: New Zealand; AU: Australia; TZ: Tasmania; NC: New Caledonia; PNG: Papua-New Guinea. Subgen: Nothofagus’ subgenera. Sp: Nothofagus’ species. Bio2: Mean Diurnal Range; Bio3 : Isothermality; Bio4: Temperature Seasonality; Bio5: Max Temperature of Warmest Month; Bio6: Min Temperature of Coldest Month; Bio7: Temperature Annual Range; Bio8: Mean Temperature of Wettest Quarter; Bio9: Mean temperature of Driest Quarter; Bio13: Precipitation of Wettest Month; Bio 14: Precipitation of Driest Month; Bio15: Precipitation Seasonality; Bio16: Precipitation of Wettest Quarter; Bio 17: Precipitation of Driest Quarter. AUC: area under the receiving operating characteristic curve. L.F. Hinojosa et al. Climatic Niche in Nothofagus 14