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A macroevolutionary role for chromosomal fusion and fission in Erebia butterflies

Augustijnen, Hannah,Bätscher, Livio,Cesanek, Martin,Chkhartishvili, Tinatin,Dincă, Vlad,Iankoshvili, Giorgi,Ogawa, Kota,Vila, Roger,Klopfstein, Seraina,de Vos, Jurriaan M.,Lucek, Kay

Abstract

H.A. was supported by the Burckhardt-Bürgin Foundation and the Swiss National Science Foundation (SNSF) project: Genomic rearrangements and the origin of species (310030_184934) awarded to K.L. K.L. was further supported by the SNSF Eccellenza project: The evolution of strong reproductive barriers toward the completion of speciation (PCEFP3_202869). J.M.d.V. was supported, in part, by SNSF grant 310030_185251. R.V. was supported by grant 2021 SGR 00420 from the Departament de Recerca i Universitats, Generalitat de Catalunya, and by Project PID2022-139689NB-I00 funded by MCIN/AEI/10.13039/501100011033 and by ERDF, EU. V.D. was supported by the Academy of Finland (Academy Research Fellow, decisions nos. 324988 and 352652). K.O. was supported by JSPS KAKENHI grant number JP21K15165.

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Augus ijnen e al., Sci. Ad . 10, eadl0989 (2024) 17 Ap il 2024 Science Ad AnceS | ReSeARch AR icle 1 o 13 EVOLUTIONARY BIOLOGY A mac oe olu iona y ole o ch omosomal usion and ission in E ebia bu e lies Hannah Augus ijnen1*, Li io Bä sche 1, Ma in Cesanek2, Tina in Chkha ish ili3, Vlad Dincă4, Gio gi Iankosh ili3, Ko a Ogawa5,6, Roge Vila7, Se aina Klop s ein8,9, Ju iaan M. de Vos1, Kay Lucek1,10* The impac o la ge- scale ch omosomal ea angemen s, such as usions and issions, on specia ion is a long- s anding conund um. We assessed whe he bu s s o change in ch omosome numbe s esul ing om ch omo- somal usion o ission a e ela ed o inc eased specia ion a es in E ebia, one o he mos species- ich and ka yo ypically a iable bu e ly g oups. We es ablished a genome- based phylogeny and used s a e- dependen bi h- dea h models o in e ajec o ies o ka yo ype e olu ion. We demons a ed ha a es o anagene ic ch o- mosomal changes (i.e., along phylogene ic b anches) exceed cladogene ic changes (i.e., a specia ion e en s), bu , when cladogene ic changes occu , hey a e mos ly associa ed wi h ch omosomal issions a he han usions. We ound ha he ela i e impo ance o usion and ission di e s among E ebia clades o di e en ages and ha es- pecially in younge , mo e ka yo ypically di e se clades, specia ion is mo e equen ly associa ed wi h cladoge- ne ic ch omosomal changes. O e all, ou esul s imply ha ch omosomal usions and issions ha e con as ing mac oe olu iona y oles and ha la ge- scale ch omosomal ea angemen s a e associa ed wi h bu s s o species di e si ica ion. INTRODUCTION The e olu ion o ba ie s o gene low is a c i ical equi emen o he p og ess o specia ion (1). Al hough se e al ba ie s may con ibu e o he p ocess, hei ela i e impo ance o en emains unknown, es- pecially a a mac oe olu iona y scale (2). Ch omosomal specia ion heo y sugges s ha la ge- scale ch omosomal ea angemen s, such as usions and issions, a e able o p omo e specia ion. They may allow o he buildup o gene ic incompa ibili ies be ween lineages ei he by causing hyb id dys unc ion (3, 4) o by supp essing ecombina ion in ea anged sec ions o he genome (5–7). The ele ance o ch omo- somal specia ion has been c i icized because o he expec ed “unde - dominance” o ch omosomal ea angemen s, whe eby s ong hyb id i ness disad an ages ensu e ha ixa ion o no el ka yo ypes is di i- cul , ende ing ba ie o ma ion unlikely (5, 6). Con e sely, i he e - ec s o ch omosomal ea angemen s on hyb ids we e mino , hen ixa ion would be possible, bu he esul ing ba ie s would emain shallow (5, 6). These heo ies we e de eloped o monocen ic ch o- mosomes, whe eas he ch omosomes o se e al majo o ganismal g oups, such as bu e lies and sedges (8), a e holocen ic, i.e., hey ha e cen ome e- like s uc u es sp ead ac oss hei ch omosomes a he han concen a ed in a single cen ome e (9). Holocen ic ch omosomes may be mo e likely o o e come he a o emen ioned unde dominance pa adox, as ea anged ch omo- somes can e ain kine ocho e unc ionali y and so lead o he c ea ion o meio ic mul i alen s ha a e only sligh ly dele e ious in hyb ids (9–11). C osses be ween closely ela ed holocen ic species wi h di - e en ka yo ypes may emain iable (11) and do no necessa ily esul in ep oduc i e isola ion (10, 12), al hough his may no be he case when sex ch omosomes a e ea anged (13). In addi ion, some holo- cen ic clades ha e e ol ed mechanisms o acili a e p ope ch omo- some seg ega ion e en when ch omosomes a e ea anged (14, 15), which has been sugges ed o p omo e ch omosomal specia ion (9). Empi ical e idence o a link be ween specia ion and ch omosomal ea angemen s, especially o ch omosomal usions and issions, is spa se o bo h mono- and holocen ic clades (8, 16). Howe e , he ac ha many holocen ic g oups wi hin plan s and in e eb a es a e e y species- ich sugges s ha ch omosomal ea angemen s could ha e d i en di e si ica ion in some o hem (9, 17). Lepidop e a is one o he la ges axonomic g oups wi h holocen- ic ch omosomes, comp ising mo e han 160,000 species o bu e - lies and mo hs (18). While some gene a wi hin Lepidop e a a e ex emely di e se in ch omosome numbe s, some imes di e ing by a coun o mo e han 200 e en wi hin a single genus (19, 20), mos o h- e s ha e conse ed ch omosome numbe s, o en close o he in e ed ances al ka yo ype [haploid numbe (n)=31]. Compa a i e phylo- gene ic analyses indica e a posi i e associa ion be ween he a e o specia ion and ka yo ype e olu ion o se e al o he mos ka yo ypi- cally di e se bu e ly gene a (16). E ebia is one o he mos speciose o all Palea c ic bu e ly gene a, consis ing o a ound 90 o 100 species ha mainly inhabi cold moun- ainous egions, wi h he majo i y o di e si y ound in Eu ope, whe e closely ela ed species o en o m na ow zones o seconda y con ac wi h li le gene low (21, 22). No ably, E ebia is also one o he gene a wi h he highes known ka yo ype di e si y among bu e lies (23), al hough his di e si y di e s be ween clades wi hin he genus. Mos ka yo ypic a ia ion can be ound in he compa a i ely young ynda- us clade (n=8 o 51) (Fig.1B and ableS1), whe e phylogene ic ela- ionships ha e emained unclea (24). As ynda us clade species a e mos ly ound in moun ainous egions (23), glacial ange expansions 1depa men o en i onmen al Science, Uni e si y o Basel, 4056 Basel, Swi ze - land. 2Slo ak en omological Socie y, Slo ak Academy o Sciences, B a isla a 1, Slo akia. 3ins i u e o ecology, ilia S a e Uni e si y, bilisi 0162, Geo gia. 4ecology and Gene ics Resea ch Uni , Uni e si y o Oulu, 90570 Oulu, Finland. 5Facul y o Social and cul u al S udies, Kyushu Uni e si y, Fukuoka 819- 0395, Japan. 6insec Sciences and c ea i e en omology cen e , Kyushu Uni e si y, Fukuoka 819- 0395, Japan. 7ins i u de Biologia e olu i a (cSic- Uni . Pompeu Fab a), 08003 Ba celona, Spain. 8ins i u e o ecology and e olu ion, Uni e si y o Be n, 3012 Be n, Swi ze land. 9li e Sciences, na u al his o y Museum Basel, 4051 Basel, Swi ze land. 10ins i u e o Biology, Uni e si y o neuchâ el, 2000 neuchâ el, Swi ze land. *co esponding au ho . email: hannah. augus ijnen@ uni . ch (h.A.); kay. lucek@ unine. ch (K.l.) copy igh © 2024 he Au ho s, some igh s ese ed; exclusi e licensee Ame ican Associa ion o he Ad ancemen o Science. no claim o o iginal U.S. Go e nmen Wo ks. dis ibu ed unde a c ea i e commons A ibu ion noncomme cial license 4.0 (cc BY- nc). Downloaded om h ps://www.science.o g a Cen o de Biologia Molecula Se e o Ochoa on No embe 11, 2024 Augus ijnen e al., Sci. Ad . 10, eadl0989 (2024) 17 Ap il 2024 Science Ad AnceS | ReSeARch AR icle 2 o 13 and con ac ions [e.g., (25)] may ha e led o popula ion bo lenecks and so p omo ed he ixa ion o he clade’s la ge a ie y o ea anged ka yo ypes h ough d i , as has been ound o o he bu e lies (26). He e, we le e aged ka yo ype di e si y ac oss E ebia o es o i s ole in species di e si ica ion. Speci ically, we i s quan i ied he o e all impac o ch omosomal usion and ission on di e si ica ion in E ebia using phylogenomic in e ence and Bayesian s a e- dependen bi h- dea h models. We hen assessed he associa ion be ween di e - si ica ion and ch omosomal usion and ission ac oss E ebia clades o di e en ages and ka yo ype di e si y. We hypo hesized ha ch o- mosomal specia ion has played a subs an ial ole in he di e si ica- ion o E ebia and ha mo e ka yo ypically di e se clades show an Fig. 1. Sample dis ibu ion and ela ionships wi hin he Palea c ic genus E ebia. (A) Map o he no he n hemisphe e indica ing sampling loca ions o E ebia specimens used, colo ed by clade. (B) Known ch omosome numbe s o E ebia species, g ouped by clade [ om (21)]. (C) ime- calib a ed phylogeny o E ebia calcula ed in M Bayes. he ossil V. ame indica was used o calib a e he oo o he ee (i.e., s em lineage o Sa y ini), while he ossil L. co bie i was placed a he c own node o Sa y ini. clade names a e based on (21) wi h he excep ion o medusa and plu o. Fo each clade a ep esen a i e pheno ype is shown. F om op o bo om, hese a e E ebia medusa, E ebia plu o, E ebia p onoe, E ebia epiph on, E ebia ynda us, E ebia ligea, E ebia magdalena, E ebia embla, and E ebia pa menio. Downloaded om h ps://www.science.o g a Cen o de Biologia Molecula Se e o Ochoa on No embe 11, 2024 Augus ijnen e al., Sci. Ad . 10, eadl0989 (2024) 17 Ap il 2024 Science Ad AnceS | ReSeARch AR icle 3 o 13 inc eased signal o ch omosomal changes and highe associa ed spe- cia ion a es. RESULTS The di e si ica ion o E ebia Al hough app oxima ely 90 o 100 E ebia species a e ecognized, he phylogene ic esolu ion o o me s udies on E ebia was limi ed, espe- cially o e olu iona y younge axa, as hese s udies included ei he ew genes (21) o ew species (27). Using whole- genome esequencing da a o 82 E ebia species, 57% o which a e ka yo yped (Fig.1, A and B, and ableS1), we cons uc ed a nea ly ully esol ed species- le el coalescen - based phylogeny based on 2920 indi idual maximum like- lihood (ML) gene ees ( ig.S1). B anch suppo was e y high o e all (>0.9 ASTRAL consensus o 96.5% o all nodes), and we u he alida ed he ela ionships among axa ollowing (28) ( igs.S2 o S6). We used he esul ing opology o cons ain a molecula clock da ing analysis in M Bayes using ossil calib a ions o he s em and c own nodes o Sa y ini and a subse o genes selec ed o minimal missing da a, especially among ou g oups (Fig.1C). We con i med he mono- phyly o p e iously de ined (21) clades ynda us [2.41 million yea s (Ma) ago; 95% highes pos e io densi y (HPD) in e al, 1.18 o 3.43 Ma ago], epiph on (2.47 Ma ago; 95% HPD, 1.49 o 4.21 Ma ago), and p onoe (3.10 Ma ago; 95% HPD, 2.07 o 4.98 Ma ago), as well as he classic axonomic clades (29) ligea (3.60 Ma ago; 95% HPD, 2.14 o 5.81 Ma ago), medusa (3.08 Ma ago; 95% HPD, 1.87 o 5.38 Ma ago), and plu o (2.94 Ma ago; 95% HPD, 1.64 o 4.93 Ma ago). We es- ima ed he age o E ebia o be 20.16 Ma old (95% HPD, 12.98 o 31.63 Ma), wi h he i s majo spli be ween he mos ly non- Eu opean embla, magdalena, and pa menio clades and all o he E ebia a 7.14 Ma ago (95% HPD, 4.62 o 11.77 Ma ago). Cladogenesis and ch omosomes We i ed a Ch omoSSE model (30) o decompose a es o ch omo- somal usion and ission in o hei anagene ic (ch omosomal change along a b anch) and cladogene ic (ch omosomal change a a specia- ion e en ) componen s (Figs.2 and 3). Ch omoSSE in e s anagene ic pa ame e s h ough a con inuous- ime Ma ko p ocess based on a Q ma ix, which desc ibes ins an aneous a es o change in e ms o ch omosome numbe s (30). Cladogene ic pa ame e s, de ined as a es o cladogenesis (i) wi h ch omosomal usions, (ii) wi h ch omo- somal issions, and (iii) wi hou ch omosomal change, a e es ima ed ia a bi h- dea h p ocess (30). Ou models, unless o he wise speci- ied, a e based on he hypo hesis ha ch omosomal usions and is- sions e ol e bo h ana- and cladogene ically. We ound ha ch omosomal changes h ough anagene ic usion (0.636 e en s pe species pe million yea s; 95% HPD, 0.134 o 1.118) occu ed a a highe a e han anagene ic ission (0.212 e en s pe species pe million yea s; 95% HPD, 0.002 o 0.550; Fig.3 and a- bleS2). Howe e , mos in e ed specia ion (cladogene ic) e en s in E ebia coincide wi h ch omosomal change, ei he wi h cladogene ic ch omosomal usion (0.196 e en s pe species pe million yea s; 95% HPD, 0.074 o 0.340) o wi h cladogene ic ission (0.328 e en s pe species pe million yea s; 95% HPD, 0.056 o 0.561; Fig.3), while he specia ion a e wi hou ch omosomal change was lowe (0.127 e en s pe species pe million yea s; 95% HPD, 0.001 o 0.320). The ela i e ex inc ion a e ac oss E ebia was 0.273 e en s pe species pe million yea s (95% HPD: 0.006–0.511) and o al specia ion (summed specia- ion a es o cladogene ic usion, cladogene ic ission, and wi hou ch omosomal change) was 0.651 e en s pe species pe million yea s (95% HPD, 0.471 o 0.839). We in e ed ha he ka yo ype a he oo o E ebia was likely n=22 o 23 (Fig.2). To explo e he in luence o he oo alue, we epea ed his analysis cons aining he oo ka yo ype o n= 29, which is he modal ka yo ype o E ebia and he ch omosome numbe o i s closes ela i es (31). We ob ained e y simila pa ame e alues whe he we es ima ed o cons ained he oo alue, al hough ixing he oo a n=29 led o a highe es ima ed a e o anagene ic usion ( ableS3). Simila esul s we e ob ained when cons aining he oo alue o n=29 o 33 ( ableS3), he eby allowing i o a y a ound he ances al ka yo ype o all bu e lies (32). Consequen ly, by es ima ing he oo alue, we ob ained conse a i e es ima es. To examine he scena io whe e ch omosomal usions and is- sions would no con ibu e o specia ion in E ebia, we i ed an al- e na i e Ch omoSSE model whe e specia ion (cladogenesis) was cons ained o be un ela ed o ch omosomal change, wi h usions and issions e ol ing only by anagenesis ( able S3). Ou ini ial model p o ides a be e i o he da a han his al e na i e ( a- ble S4), again con i ming ha usions and issions e ol e bo h cladogene ically and anagene ically. Clade- speci ic ch omosomal changes To es whe he ana- o cladogene ic ch omosomal change a es would be highe in clades ha show a highe ka yo ype di e si y (Fig.1B), we an Ch omoSSE o he six clades wi h su icien ch o- mosome coun da a and species (Figs.1B and 4A and ableS5). We ound ha he a es o bo h ana- and cladogene ic ch omosomal change di e ed ac oss clades unde Ch omoSSE: Anagene ic usions di e ed signi ican ly among clades (K uskal- Wallis es , χ25=3303.5, P<0.001; pe mu a ion es wi h 1000 i e a ions, P<0.001; Fig.4B), wi h pos e io dis ibu ion means anging om compa a i ely low, 0.084 (ligea), o mode a e, 0.296 (p onoe), e en s pe species pe mil- lion yea s. This was also ue o anagene ic issions (χ25=1582.6, P<0.001; pe mu a ion es , P<0.001; Fig.4C), wi h mean a es be- ween 0.065 (ligea) and 0.168 (p onoe) e en s pe species pe million yea s. To al anagene ic ch omosomal change, de ined as he sum o a es o anagene ic usions and issions, anged om 0.148 (ligea) o 0.464 (p onoe) e en s pe species pe million yea s, which, o all clades, is less han he 0.848 (95% HPD, 0.420 o 1.295) ound o he o e all Ch omoSSE analysis o E ebia ( ableS2). The a e o cladogene ic ch omosomal usion showed a highe de- g ee o di e en ia ion among clades han o he ana- o cladogene ic pa ame e s (χ25=6958.5, P<0.001; pe mu a ion es , P<0.001; Fig.4F), anging om 0.327 (epiph on) o 1.263 ( ynda us) e en s pe species pe million yea s. The a e o cladogene ic ch omosomal ission was likewise a iable be ween clades (χ25=2365.5, P<0.001; pe mu a ion es , P<0.001; Fig.4G), anging be ween 0.113 (ligea) and 0.594 ( ynda us) e en s pe species pe million yea s. The summed a es o cladogene ic usion and ission anged om 0.538 (ligea) o 1.856 ( ynda us) e en s pe species pe million yea s. These a es we e gene ally highe han o o e all E ebia (0.524 e en s pe species pe million yea s), bu he pos e io dis ibu ions o mos clades o e lap wi h he 95% HPD (0.304 o 0.783) o he o e all pa- ame e ( ableS2). The excep ion was he ka yo ypically di e se yn- da us clade (95% HPD, 0.906 o 2.898), whose a e exceed ha o E ebia. While he pa ame e alues we e e y simila be ween some clades, hei p opo ional con ibu ions o a es o specia ion di e (Fig.4). Fo example, medusa, plu o, and epiph on show simila a es Downloaded om h ps://www.science.o g a Cen o de Biologia Molecula Se e o Ochoa on No embe 11, 2024 Augus ijnen e al., Sci. Ad . 10, eadl0989 (2024) 17 Ap il 2024 Science Ad AnceS | ReSeARch AR icle 4 o 13 Fig. 2. Summa y o he ch omosome e olu ion model o E ebia, implemen ed in Ch omoSSE. es ima ed ances al ch omosome numbe s o E ebia, in e ed using he phylogenomic opology o ig.S1. ch omosome numbe s a e indica ed p opo ionally by he colo o he pie cha s a he b anch nodes. he pie cha s a he “shoul- de s” o each node ep esen he in e ed ch omosomal s a e immedia ely a e a specia ion e en . he wo in e ed ch omosome numbe s wi h highes pos e io dis i- bu ion o he ances o o each clade a e depic ed a op o below he node ha s a s ha clade. Fo deepe nodes wi hin he ee, he econs uc ed ances al cha ac e s a es a e likewise p esen ed. Fo each ex an species in he phylogeny, he ka yo ype is shown be o e he name. When he ka yo ype o a species is no known, he spe- cies is deno ed wi h a “?.” clades a e named as in Fig.1. he pos e io p obabili ies o econs uc ed ances al ch omosome s a es a e isualized in ig.S7. Downloaded om h ps://www.science.o g a Cen o de Biologia Molecula Se e o Ochoa on No embe 11, 2024 Augus ijnen e al., Sci. Ad . 10, eadl0989 (2024) 17 Ap il 2024 Science Ad AnceS | ReSeARch AR icle 5 o 13 o cladogene ic ch omosomal issions bu hey accoun o 19.8, 18.9, and 30.0% o he o al cladogene ic e en s, espec i ely. Specia ion a es (cladogenesis) wi hou ch omosomal change di - e ed among clades (χ25= 4144.1, P< 0.001; pe mu a ion es , P<0.001; Fig.4E) anging om 0.145 (p onoe) o 0.423 (ligea) e en s pe species pe million yea s bu ne e accoun ed o a majo i y o he o al specia ion in a clade ( hough nea ly so in ligea; Fig.4, E and F, and ableS2). Rela i e ex inc ion a es we e highes o ynda us a 0.745 and a ied be ween clades (χ25= 5089.6, P< 0.001; pe mu a ion es , P<0.001; Fig.4D), wi h he lowes a es o p onoe (0.197) and ligea (0.252). To al specia ion ela ed di ec ly o a es o cladogene ic e en s and likewise a ied be ween clades (χ25=5807.1, P<0.001; pe mu a- ion es , P<0.001; Fig.4H), wi h ynda us ha ing he highes deg ee o o al specia ion (2.191; 95% HPD, 1.283 o 3.363 e en s pe species pe million yea s). The co ela ion be ween ela i e ex inc ion and o- al specia ion was 0.38 ( 1,14998=50.7, P<0.001). We also epea ed his analysis while equalizing he maximum ch omosome numbe allowed in each clade (n=56) o minimize he po en ial e ec s o di e ing Q ma ices be ween models. The esul ing pa ame e es ima es a e la gely simila o he models whe e maxi- mum ch omosome numbe s we e allowed o be ailo ed o each clade, wi h all 95% HPD o e lapping ( ableS6). Howe e , unning all clades wi h 56 maximum ch omosomes does lead o lowe es ima es o o al specia ion ( ableS6) and o lowe es ima es o cladogene ic ch omo- somal usion. None heless, in all cases, he model wi h 56 maximum ch omosomes was no p e e ed o e he o iginal one ( ableS7). As o he o e all phylogeny, we i ed al e na i e Ch omoSSE models o each clade, whe e usions and issions we e cons ained o be only anagene ic. Fo epiph on, medusa, plu o, and, especially, ynda us, he o e all model wi h combined cladogene ic and anagen- e ic e olu ion o ch omosome numbe s was p e e ed ( ableS8). In p onoe, whe e anagene ic changes a e mos equen o all clades ( a- bleS2), bu cladogene ic usions a e likewise common, he e idence is mixed, wi h Akaike’s in o ma ion c i e ion h ough Ma ko chain Mon e Ca lo (AICM) p e e ing he model whe e specia ion does no ela e o ch omosomal change and Bayes ac o s (BFs) inding no di - e ence be ween model i s ( ableS8). Fo ligea, he clade wi h he leas ch omosomal a ia ion (Fig.1B and ableS1), he al e na i e model was p e e ed ( ableS8). A ale o wo models To assess o which deg ee he combined in e ence o specia ion and ex inc ion a es in Ch omoSSE migh a ec ou es ima ions o cla- dogene ic and anagene ic pa ame e s, we alida ed he esul s o Ch omoSSE by ca ying ou simila analyses in Ch omEVOL (33) ollowing (30), which allows o model usion- and ission- associa ed cladogene ic changes bu does no include an ex inc ion pa am- e e . We expec ed po en ial di e ences be ween he models in clades wi h highe ex inc ion and specia ion a es. Al hough he esul s o Ch omoSSE and Ch omE ol we e la gely simila o nea ly all clades ( ableS9, Fig.4, and ig.S8), he ma ginal likeli- hoods and AICMs o Ch omE ol models we e gene ally highe , likely owing o a la ge pa ame e space o Ch omoSSE compa ed o Ch omEVOL. The di e ence in ma ginal likelihood was mo e p onounced o he o e all ee han o indi idual clades (di e ence in BFs anging om o 10.002 (plu o) o 40.411 (medusa); ablesS4 and S10). In con as o he o he E ebia clades, we ound ha he Ch omoSSE model leads o a be e ela i e i o he da a han he Ch omEVOL one (BF=8.857, AICM=34.025) o ynda us, he clade wi h he highes in e ed ex inc ion a es (Fig.4D). An ex- plana ion o he di e ence be ween Ch omoSSE and Ch omEVOL could be ha simple models wi h ewe pa ame e s (Ch omEVOL) esul in highe ma ginal likelihoods han mo e complex models 0.00.3 0.60.9 1.21.5 1.82.1 E en s pe species pe Ma To al specia ion Rela i e ex inc ion Specia ion (cladogenesis) wi hou ch omosomal change Specia ion (cladogenesis) wi h ch omosomal usion Specia ion (cladogenesis) wi h ch omosomal ission Anagene ic ch omosomal usion Anagene ic ch omosomal ission Fig. 3. A summa y o he pos e io dis ibu ions o in e ed Ch omoSSE pa ame e s o he o e all E ebia analysis. Shown a e he pos e io densi ies pe pa ame e , he aw da a poin s, and he 95% hPd in e al as p esen ed by he bold black line unde nea h each densi y plo ( ableS2). All pa ame e a es a e exp essed in e en s pe species pe million yea s (Ma). Downloaded om h ps://www.science.o g a Cen o de Biologia Molecula Se e o Ochoa on No embe 11, 2024 Augus ijnen e al., Sci. Ad . 10, eadl0989 (2024) 17 Ap il 2024 Science Ad AnceS | ReSeARch AR icle 6 o 13 0.00 0.25 0.50 0.75 1.00 0.0 0.4 0.8 1.2 1.8 2.0 E en s pe species pe Ma A Cladogenesis wi hou ch omosomal change E Ch omoSSECh omEVOL Cladogene ic ch omosomal usions F Ch omoSSECh omEVOL 0.0 0.25 0.50 0.75 1.00 1.25 E en s pe species pe Ma Cladogene ic ch omosomal issions G Ch omoSSECh omEVOL 0.0 0.5 1.0 1.52.0 2.5 3.0 H 0.0 0.5 1.0 1.52.0 2.5 3.03.5 4.0 To al specia ion E en s pe species pe Ma 0.0 0.2 0.4 0.6 0.8 1.0 Rela i e ex inc ion D E en s pe species pe Ma Anagene ic ch omosomal usions B Ch omoSSE Ch omEVOL 0.0 0.2 0.4 0.6 0.8 medusa plu o p onoe epiph on ynda us ligea C Anagene ic ch omosomal issions 0.0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 Ch omoSSE Ch omEVOL E en s pe species pe Ma E en s pe species pe Ma Rela i e e en s pe species pe Ma Rela i e e en s pe species pe Ma Rela i e e en s pe species pe Ma 0.00 0.25 0.50 0.75 1.00 0.00 1.00 2.00 0.00 0.25 0.50 0.75 1.00 0.00 0.25 0.50 0.75 1.00 E en s pe species pe Ma E en s pe species pe Ma E en s pe species pe Ma Fig. 4. Summa y o ana- and cladogene ic ances al ch omosome es ima ions o six E ebia clades. (A) O e iew o he phylogeny o e ebia wi h ele an clades highligh ed. (B o H) dis ibu ions o he pos e io p obabili y es ima es o (B) anagene ic usions, (c) anagene ic issions, (d) ela i e ex inc ion a es, (e) cladogene ic changes un ela ed o ch omosomal change, (F) cladogene ic ch omosomal usions, (G) cladogene ic ch omosomal issions, and (h) o al specia ion a es. Fo (B) and (c) and (e) o (G), compa isons be ween s anda dized pa ame e es ima ions o clade speci ic s a e- dependen bi h- dea h models (ch omoSSe) and bi h- dea h indepen- den models (ch ome Ol) a e shown. each do indica es he mean o he pos e io p obabili y space. All pa ame e a es a e exp essed in e en s pe species pe million yea s. An al e na i e isualiza ion, pe clade, no pe pa ame e , is gi en in ig.S8. Downloaded om h ps://www.science.o g a Cen o de Biologia Molecula Se e o Ochoa on No embe 11, 2024 Augus ijnen e al., Sci. Ad . 10, eadl0989 (2024) 17 Ap il 2024 Science Ad AnceS | ReSeARch AR icle 7 o 13 which may su e om o e pa ame e iza ion, pa icula ly in ela- i ely small da ase s. In clades wi h low o medium in e ed ela i e ex inc ion a es (e.g., medusa), he mo e complex Ch omoSSE model was no p e e ed o e he ela i ely simple Ch omE ol. In ynda us, by con as , i appea s ha modeling ex inc ion in an- dem wi h ch omosomal e olu ion as Ch omoSSE was designed o do was su icien o o e come he po en ial issue o o e pa ame- e iza ion. Because Ch omE ol es ima es cladogene ic pa ame e s as p o- po ions o he o al a e o cladogene ic change, cladogene ic pa am- e e s om he Ch omoSSE analysis we e di ided by he mean o al specia ion a e (Fig.4G), allowing us o compa e a es be ween mod- els. Fo he en i e ee, a es o cladogenesis wi hou ch omosomal change, cladogene ic usions and cladogene ic issions o e lapped in hei pos e io dis ibu ions, bu pos e io means di e ed be ween he models (K uskal- Wallis and pe mu a ion es s, all P< 0.001; ig.S9), in cong uence wi h he ela i ely high di e ence be ween BFs. Howe e , he a es o ch omosomal ission–associa ed specia- ion emained highe han hose o ch omosomal usion unde bo h models ( ableS9). Ra es o anagene ic issions showed a highe o e - lap in pos e io dis ibu ion and did no di e signi ican ly in means (χ25=0.017, P=0.896; pe mu a ion es , P=0.208; ig.S9). Ra es o anagene ic usions did di e be ween models (χ25= 2925.2, P<0.001; pe mu a ion es , P<0.001; ig.S9). This di e ence was mos likely d i en by ynda us clade (see Fig.4B) and may be ela ed o i s high ela i e ex inc ion a es. To assess he e ec s o missing ka yo ype da a on ou in e ences, we an Ch omoSSE and Ch omEVOL again, using simila pa ame- e s, on a da ase limi ed o axa o which ch omosome numbe s a e a ailable ( ig.S10). The esul s o Ch omEVOL and Ch omoSSE o his da ase we e highly cong uen wi h ou o e all E ebia analyses ( ableS3). Fo Ch omoSSE, howe e , ch omosomal issions ended o be assigned mo e as anagene ic ( ableS3), which is consis en wi h analyses using less comple e phylogenies (34). DISCUSSION Compa ed o o he ea angemen s, such as in e sions, much mo e emains unknown abou he ole o ch omosomal usion and ission in specia ion (8). Theo y p edic s ha usions and issions could ha e majo impac s on he specia ion p ocess (3, 5), pa icula ly in species whose ch omosomes a e holocen ic and he e o e may no ini ially be as s ongly a ec ed by he unde dominance pa adox (8, 11, 15). He e, we ound phylogenomic e idence o an associa ion o ch omosomal usion and ission wi h highe specia ion a es a mac oe olu iona y scale, p o iding indi ec e idence o hei in ol emen du ing specia- ion. Ch omosome- associa ed cladogene ic e en s we e p e alen in E ebia and we e associa ed wi h highe a es o specia ion han specia ion wi hou ch omosomal change (Fig.2B), ou pe o ming al- e na i e models wi hou ch omosomal change ( ableS4). Such clado- gene ic e en s coincide wi h spli s be ween lineages and, in heo y, ep esen cases whe e ch omosomal ea angemen s may ha e a mo e causa i e in ol emen in specia ion (30). Al e na i ely, cladogene ic ch omosomal e en s could ep esen a di ec consequence o specia- ion i he buildup o ep oduc i e isola ion sepa a es di e ging ka yo- ypical lineages wi hin he same popula ion (8). Howe e , a causal ole o ch omosomal usions and issions may be especially likely when hey hemsel es ac as in insic ba ie s o gene low, e.g., by esul ing in hyb id dys unc ion (3, 4), by physically b inging oge he si es unde selec ion (35), o i sex ch omosomes a e in ol ed (13). Ch o- mosomal usions and issions may he e o e accompany apid di e si- ica ion o lineages in o species adia ions, e.g., (36), o ins ance, he e, in E ebia (21). F om a phylogene ic pe spec i e, ch omosome- associa ed specia- ion should mainly conce n cladogenesis, i.e., he spli ing o an an- ces al species in o wo new lineages. Howe e , ecen heo y p edic s ha anagene ic ch omosomal changes could also con ibu e o spe- cia ion by g adually building up di e en ia ion in ka yo ypes o e ime, po en ially leading o inc eased ep oduc i e isola ion (8). Mos changes in ch omosome numbe in he o e all E ebia phylogeny ap- pea o ha e occu ed anagene ically (Fig.2). Ch omosomal usion and ission could he e o e ac as ba ie s o gene low, simila o o h- e ea angemen s (35), including in e sions, e.g., (37). Fusion and ission could supp ess ecombina ion wi hin o a ound ea anged sec ions o he genome be ween hyb ids (38) and so p e en he b eakup o linkage disequilib ium be ween locally co- adap ed genes (5), p omo ing he g adual accumula ion o di e ences h ough ime (39, 40). Specia ion may hen be comple ed h ough addi ional p o- cesses (41), such as ein o cemen upon seconda y con ac , as has been sugges ed o o he bu e lies (42). Ou analyses sugges ha he e olu iona y impac s o ch omo- somal usions and issions di e , as usions we e mo e likely o be ana- gene ic ac oss he en i e E ebia phylogeny. Con e sely, issions we e mo e likely o be associa ed wi h cladogene ic e en s, leading o high- e cladogene ic specia ion a es when issions a e in ol ed (Fig.2). Reduc ions in ch omosome numbe h ough usion e en s we e mo e common han issions in E ebia, as well as o he g oups o bu e lies (16) and holocen ic o ganisms, e.g., (43). Ch omosomal issions, al- hough a e , could he e o e be associa ed wi h highe specia ion a es i hey mo e o en esul in somewha dele e ious meio ic mul i- alen s (16, 44). Mo e s udies a e needed o con i m his hypo hesis, and his e ec may be pa ially mi iga ed in Lepidop e a due o hei holocen ic ch omosomes (15, 45). Sho e ch omosomes ha e also been shown o ha e an inc eased likelihood o be in ol ed in usions (32), sugges ing ha longe ch omosomes may be mo e e olu iona y s able. The appa en highe e olu iona y s abili y o used ch omo- somes and he ins abili y o issions could explain why clades wi h highe ch omosome numbe s show highe cladogene ic specia ion a es in E ebia (Figs.2 and 4) and o he bu e lies (16). The highe o e all deg ee o anagene ic usions obse ed in his s udy migh con- ibu e o he buildup o ep oduc i e isola ion by g adually educing ecombina ion a es, as has been ound in mice (46) and o he bu - e lies (47). Genome- wide c ossing- o e a es co espondingly seem o be conside ably highe when ch omosomes a e sho o e ol e o become sho e (48), bu see (49). While he e a e some examples o s udies ocusing on he mac o- e olu iona y impac o ch omosomal usions and issions, as well as o he ea angemen s (50–52), unde s anding pa e ns o ch omosome- associa ed specia ion may equi e addi ional analysis a a ine axo- nomic scale (43). He e, we assessed he ela i e con ibu ions o ch omosomal usion and ission be ween clades o di e ing ages and ka yo ype di e si y, o assess he impac o hese ea angemen s on specia ion. We iden i ied a con inuum o ch omosome- associa ed spe- cia ion a es, anging om he young, ka yo ypically e y di e se yn- da us clade ha showed he highes a es o specia ion ela ed o ch omosomal change (Fig.4 and ig.S8) o ka yo ypically mo e con- se ed clades, such as ligea, whe e he p opo ion o specia ion un e- la ed o ch omosomal change was much highe (Fig.4E) and a model Downloaded om h ps://www.science.o g a Cen o de Biologia Molecula Se e o Ochoa on No embe 11, 2024 Augus ijnen e al., Sci. Ad . 10, eadl0989 (2024) 17 Ap il 2024 Science Ad AnceS | ReSeARch AR icle 8 o 13 wi hou ch omosomal specia ion was e en p e e ed ( ableS8). O he clades ell along his con inuum, whe e a es o specia ion wi h ch o- mosomal usion we e gene ally high and anagenesis appea s o be less impo an a he subclade le el han o he o e all ee (Fig.4). No a- bly, he clades plu o and p onoe, which a e second o ynda us in ch o- mosome a iabili y (Fig. 1B), also show he lowes p opo ion o specia ion ha is no d i en by ch omosomal usion and ission (Fig.4E), al hough hey emain behind ynda us in absolu e alues ( ableS2). The high ka yo ype di e si y and associa ed high specia ion a es o he ynda us clade may, in pa , be explained by hei ecology. Spe- cies o he ynda us clade occu almos exclusi ely in Alpine a eas (23), whe eas o he E ebia clades a e ecologically mo e di e se (24, 53). Du ing glacial cycles, epea ed ange expansions and con ac- ions ac oss ela i ely small geog aphic a eas ha e caused popula ion subdi isions o many E ebia species, e.g., (54, 55), including he yn- da us clade (25). Fo he la e , d i and o he s ochas ic p ocesses could ha e p omo ed he ixa ion o no el ch omosomal ea ange- men s (56). Na u al selec ion may also ha e played a ole in he ixa- ion o usions, al hough i is no known o which deg ee (26). Fu he in es iga ion o bu e ly lineages wi h widely a ying ch omosome numbe s (16, 57) will be equi ed o de e mine he unde lying mech- anisms o he usions and issions ha a ec specia ion (8). While s a e- dependen specia ion and ex inc ion (SSE) models al- low o unp eceden ed phylogene ic insigh s in o mac oe olu iona y aspec s o specia ion (58–60), hei eliabili y has been pa ially ques- ioned (61). They may, o example, su e om excess alse- posi i e a es because shi s in di e si ica ion a es ac oss he phylogeny may be assigned o a s udied ai in an SSE model e en when hese shi s a e caused by an unde ec ed and un ela ed ai (61, 62). This could lead o an o e es ima ion o in e ed pa ame e s. Howe e , simula- ions ha e indica ed ha Ch omoSSE is mo e likely o unde es ima e, a he han o e es ima e, cladogene ic changes, implying ha ou in- e ences a e ins ead a he conse a i e (30). Fu he mo e, as he model canno de ec “c yp ic” ch omosomal ea angemen s, e.g., usion and ission e en s ha coun e balance each o he and, he e o e, do no lead o changes in ch omosome numbe , ou da a may e en ep esen an unde es ima ion o he e - ec s o ch omosomal ea angemen s on specia ion. Fo example, Mackin osh e al. (63) ound nine possible usion and ission e en s ha may ha e con ibu ed o specia ion be ween wo B en his bu - e lies ha o he wise di e li le in hei ch omosome numbe s. O he ea angemen s, such as in e sions, may simila ly a ec ch o- mosome e olu ion and e en con ibu e o specia ion (64). Howe e , ch omosome- le el assemblies o all E ebia would be equi ed o s udy hei impac in his sys em. We also highligh ha a solid axonomic amewo k, as p esen ed he e, is highly p e e able o he co ec in e p e a ion o SSE- based in e ences (34). Limi ing he da ase o only ka yo yped species e- u ns simila alues o mos pa ame e s ( ableS3) bu ends owa d highe unce ain y (la ge 95% HPD in e als) and o e es ima ion o anagene ic pa ame e s, pa icula ly issions, which is expec ed o incomple e phylogenies (34). Howe e , gi en he axonomic com- plexi y o E ebia (21), i is likely ha some c yp ic species may exis , again indica ing ha ou es ima es o di e si ica ion may be a he conse a i e. In addi ion, hyb idiza ion in E ebia is no common, and closely ela ed species end o o m e y na ow con ac zones wi h li le o no gene low, e.g., (22, 65), as is he case o o he Eu o- pean bu e lies (66). Al hough he possibili y o gene low among ou sequenced indi iduals in he dis an pas canno be ully excluded, such gene low is unlikely and would no ha e a ec ed he o e all opology o ou phylogeny. We u he con i med he alidi y o ou in e ences by i ing Ch omE ol (33) models ha do no es ima e ex inc ion and may hus no su e he same po en ial pi alls as SSE ype models. We ound e y simila esul s as o he SSE- based analyses (Figs.2B and 4), wi h he excep ion o in e ed a es o anagene ic usions in he ynda us clade, which we e es ima ed o be much highe o Ch omE ol. This di e ence may be due o he in luence o he high ela i e ex inc ion a es in his clade (Fig.4H), as Ch omE ol does no conside any unobse ed specia ion ha may ha e esul ed in ex inc ion, whe eas Ch omoSSE does (30). We u he es ima ed hidden backg ound specia ion and ex inc ion a es wi hou conside ing ch omosomal change using MiSSE (59) and ound ha , o ex an species, hese a es do no appea o a y much (Supplemen a y Me hods and igs.S12 and S13). Consequen ly, ou econs uc ion o ch omosom- al change ac oss he deepe E ebia ee is unlikely o ha e been in lu- enced by hidden specia ion. He e, we used s a e- o - he- a phylogenomic models in one o he mos ka yologically di e se g oups o bu e lies, p o iding e idence o a mac oe olu iona y impac o majo ch omosomal ea ange- men s ha equally occu in many o he animal, e.g., (51, 67) and plan (50, 52) g oups. O e all, we p o ide e idence ha specia ion a es a e highe wi h inc eased ch omosomal changes. Simila in e ences o he impac s o ch omosomal ea angemen s a e o en ca ied ou a highe axonomic le els o ac oss as e olu iona y imescales, e.g., (68, 69), po en ially masking ine- scaled pa e ns in younge clades. Ou s udy b idges hese o me in es iga ions and mic oe olu iona y s udies ha ocus on one species o compa e sibling species, e.g., (10, 51, 63, 68), by demons a ing wi hin- genus di e ences o ch omo- somal usion- and ission- ela ed specia ion. We highligh ha ch o- mosomal specia ion may be mo e ele an in clades wi h mo e di e si y in ch omosome numbe s. In his genomic e a, high- quali y e e ence genomes can be gene a ed and used o build phylogenomic amewo ks, which will enable us o u he un a el he complexi ies o ch omosomal e olu ion and specia ion. MATERIALS AND METHODS Da a collec ion Adul specimens o 83 E ebia species we e collec ed be ween 2009 and 2021 ( ableS1). Whene e possible, species we e no sampled om egions whe e hey migh hyb idize wi h o he , closely ela ed E ebia species. Bodies we e ei he s o ed in e hanol a −20°C (n=53) wi h wings sepa a ed o pinned a oom empe a u e (n=30). Fo he la - e , he wings we e cu and s o ed sepa a ely be o e DNA ex ac ion. DNA was ex ac ed om ho ax issue using a Qiagen Blood and Tis- sue ki (Qiagen AG, Homb ech ikon, Swi ze land) ollowing he s an- da d manu ac u e ’s p o ocol. Pai ed- end sequencing lib a ies we e cons uc ed a he Depa men o Biosys ems Science and Enginee - ing o ETH Zü ich in Basel, ollowed by sequencing on an Illumina No aSeq 6000. Samples we e sequenced on wo S1 low cells. Species iden i y o each specimen was con i med using an in silico DNA ba - coding app oach. In sho , we used he pipeline o (70) wi h s anda d se ings, o ex ac eads ha showed a high k- me simila i y o E ebia mi ochond ial ba code sequences. Ba code e e ence sequences o all a ailable species we e ob ained om he Ba code o Li e Da abase (www.boldsys ems.o g). Fo each indi idual, we hen pe o med a Downloaded om h ps://www.science.o g a Cen o de Biologia Molecula Se e o Ochoa on No embe 11, 2024 Augus ijnen e al., Sci. Ad . 10, eadl0989 (2024) 17 Ap il 2024 Science Ad AnceS | ReSeARch AR icle 9 o 13 de no o assembly o he il e ed eads wi h SPAdes 3.13.0 (71) and mapped he con igs back o he ba code da abase wi h Yass 1.14 (72). On he basis o he assembled ba code sequence, he species iden i y o all indi iduals in ou s udy was co ec ly assigned. Demul iplexed aw sequence eads we e p ocessed using as p (73), imming poly- G ails. Re ained eads we e mapped o he ch omosome- esol ed E ebia ligea e e ence genome (74), using bwa 0.7.17 (75). A e age mapping co e age was 38% bu a ied among species, e lec ing phylogene ic dis ance o he e e ence genome ( ig.S11). One species (E ebia a amen a ia) was omi ed because o e y low co e age (2.5%). SAM ools .1.13 (76) was hen used o e- mo e unmapped, unpai ed, o duplica ed eads. A pileup ile o each sample was gene a ed wi h BCF ools .1.12 (77) mpileup, ollowed by a ian calling in BCF ools call (78). Indi idual Va ian Call Fo ma (VCF) iles we e hen me ged and subsequen ly il e ed o emo e (i) non- biallelic single- nucleo ide polymo phisms (SNPs), (ii) inse ions and dele ions and adjacen SNPs wi hin 5base pai s (bp), (iii) SNPs wi h quali y sco e<30, (i ) SNPs wi h mo e han 80% missing da a, ( ) SNPs wi h dep hs < 4 o >25, ( i) SNPs wi h mino allele equen- cies (MAFs) < 0.03, and ( ii) SNPs alling wi hin epe i i e pa s o he genome as iden i ied by Repea Maske 4.0.9 (79). This esul ed in a da ase con aining 1.87 million SNPs om 82 E ebia samples. The aw eads o hese samples ha e been deposi ed on Na ional Cen e o Bio echnology In o ma ion (NCBI) unde he accession numbe PRJNA1000734. Ou g oup da a we e aken om ch omosome- esol ed assemblies o o he Nymphalid bu e lies ha we e publicly a ailable a he ime o analysis: he Sa y ini Pa a ge aege ia (80), Aphan opus hype an us (81), and mo e dis an ou g oups Aglais u icae (82), Vanessa a alan a (83), and Vanessa ca dui (84). To ob ain single copy o hologs (SCOs) among all assemblies, each assembly including E. ligea was anno a ed wi h WebAugus us (85, 86) in wo s eps: Fi s , gene p edic ion was un using he s anda d Augus us species pa ame e s o Heliconius melpomene. Then, pai wise SCOs be ween E. ligea and all o he spe- cies we e iden i ied wi h O ho inde (87). These SCOs we e subse- quen ly used o gene p edic ion in a second un o WebAugus us. A o al o 4505 SCOs among E. ligea and ou selec ed ou g oups we e iden i ied, o which 2920 SCOs wi h ≥20 SNPs we e e ained o downs eam analyses. Exons o each SCO we e conca ena ed in o a single coding egion o c ea e 2920 sepa a e VCF iles ex ac ed om he E ebia da ase wi h BED ools (88). VCF iles we e hen ansposed in o FASTA o ma , and he same exons we e ex ac ed o each ou - g oup species and aligned o he E ebia sequence iles. Each esul ing gene sequence ile was aligned wi h MAFFT .7.467 (89). Phylogenomic analyses ML gene ees we e es ima ed in IQTREE2 (90), which i s es i- ma es he op imal subs i u ion model o a gene alignmen h ough ModelFinde (91). Gene ees we e es ima ed wi h ul a as boo s ap app oxima ion o 1000 i e a ions. A species consensus ee was hen in e ed using coalescen me hods in ASTRAL- III (92). Be o e his analysis, b anches wi h <10% boo s ap suppo we e collapsed o imp o e he accu acy o ASTRAL- III (92). The esul ing species ee had a no malized qua e sco e o 0.64, indica ing 64% ag eemen be- ween gene ee opologies ( e lec ing an in e media e amoun o in- comple e lineage so ing) and high o e all suppo ( ig.S1). The obus ness o he phylogeny was u he alida ed ollowing (28), i.e., selec ing loci based on phylogene ically in o ma i e pa am- e e s o educe incong uency (28, 93, 94). Fi e alida ion da ase s we e c ea ed, each con aining he 600 gene ees ha (i) had he high- es a e age boo s ap in IQTREE; (ii) showed he highes clocklike- ness, indica ing how well a gene ee app oaches an ul ame ic ee o ma ion; (iii) had he lowes CG e sus AT con en s; (i ) had he highes p opo ion o pa simony in o ma i e si es; and ( ) showed he lowes mu a ion sa u a ion po en ial. Da ase s (i), (ii), and ( ) we e gene a ed wi h a modi ied ee_p ops.R sc ip om (95). Da a- se s (iii) and (i ) we e gene a ed wi h FASconCAT (96). The sa u a ion po en ial was calcula ed h ough eg ession slopes, wi h lowe mu a- ional sa u a ion po en ial indica ing a lowe deg ee o amino acid subs i u ions and a lowe sensi i i y o di e ences in e olu iona y a es (93, 97). Consensus opologies o each da ase based on IQTREE gene ees we e gene a ed wi h ASTRAL- III. The a e age no malized qua e sco e was simila o he o e all da ase wi h 0.68 ( ange, 0.61 o 0.77). Compa isons be ween opologies o he o e all da ase and he alida ion opologies indica ed only mino di e ences conce ning ela ionships wi hin clades and conce ned he placemen o E ebia ni- phonica and E ebia ae hiops, which a e no used in he clade- le el analyses. All clades used o u he analyses we e s ongly suppo ed in all alida ion da ase s ( igs.S2 o S6). The phylogeny based on he o e all da ase , he ea e e e ed o as he All gene opology, was he e o e used in downs eam analyses o cons ain da ing analyses using ossil calib a ion. Di e gence ime es ima ion Mos s a e- dependen bi h- dea h (SSE) models equi e ul ame ic ees because a es a e exp essed in ela i e o absolu e uni s o ime. The la e allows o he exp ession o s a e- dependen a es o di e - si ica ion in e ms o e en s pe species pe million yea s and is he e- o e mo e in o ma i e o in e p e . We in e ed an ul ame ic ime ee based on he 56 genes wi h <1% missing da a, o a o al o 82,923 bp, wi h he opology cons ained acco ding o he All gene opology. We chose o minimize missing da a o he da ing analysis as i occu ed p ima ily in ou g oups, which could bias b anch leng hs and ela ion- ships among ou g oups, which would, in u n, a ec he calib a ions, which we e placed among he ou g oups. No ossils a e known o E ebia and ew o Sa y ini o e all. Le he co bie i (98), which has p e iously been used o da ing Sa y ini phy- logenies (99), was he e o e selec ed. As he wo ou g oup species wi hin Sa y ini, P. aege ia and A. hype an us, span he b ead h o he clade, hei spli om E ebia coincides wi h he c own age o Sa y ini. Thus, he age o L. co bie i (25.0 Ma ago) was aken as a conse a i e minimal bound o he age o Sa y ini, wi h he median age se a 41.8 Ma ago, ollowing he in e ence o (99). The oo o he ee ep esen s he age o Nymphalidae and s em age o Sa y ini, p e iously es ima ed o be 69.4 Ma ago (59.0 o 80.2 Ma ago) (100), which was aken as he median age o his node. The minimum age o Nymphalidae was bounded using he ossil Vanessa ame indica, as i s placemen wi hin Vanessa is deba ed (101), and we conside ed placing his ossil close o he base o Nymphalidae o be he mo e conse a i e app oach. Calcula ions o he di e gence imes we e ca ied ou by node da ing in M Bayes .3.2.7 (102). Pa i ionFinde (103) was used o pa i ion he da ase and selec he pe - pa i ion bes subs i u ion models. The in gamma model o among- si e a e a ia ion was he bes model o all pa i ions, and we u he allowed o in eg a ion o e he ull gene alized ime- e e sible (GTR) subs i u ion model space. Ha d cons ain s we e placed on all nodes based on he All gene opology, wi h he clade Sa y ini cons ained o E ebia, P. aege ia, and A. hype an us o es ima e i s node age based on an o se Downloaded om h ps://www.science.o g a Cen o de Biologia Molecula Se e o Ochoa on No embe 11, 2024