2026 in paleobotany
| List of years in paleobotany |
|---|
This paleobotany list records new fossil plant taxa that were announced or described during the year 2026, as well as notes other significant paleobotany discoveries and events which occurred during the year.
Algae
Chlorophytes
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Salpingoporella vivariensis[1] |
Sp. nov |
Bucur et al. |
A member of Dasycladales. |
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|
Similiclypeina hadrianii[1] |
Sp. nov |
Bucur et al. |
Early Cretaceous (Aptian) |
A member of Dasycladales. |
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Ochrophytes
| Name | Novelty | Status | Authors | Age | Type locality | Location | Notes | Images |
|---|---|---|---|---|---|---|---|---|
|
Forticellula[2] |
Gen et sp. nov |
Valid |
Siver |
Early Eocene |
Eocene Okanagan Highlands |
A tabellariaceous fragilariophycean diatom. |
||
Rhodophytes
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Vetusceramium[3] |
Gen. et sp. nov |
Du et al. |
A member of Ceramiales belonging to the family Ceramiaceae. The type species is V. sinense. |
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Phycological research
- Mohammed et al. (2026) determine flask-shaped microfossils from the Dzhanytas Group (Kazakhstan) to be mid-Tonian in age, representing the oldest record of such microfossils reported to date, and interpret them as possible fossils of red algae.[4]
- Fossil evidence of persistence of multicellular algae belonging to the genus Wengania into the early Cambrian is reported from the Zhujiaqing Formation (Yunnan, China) by You, Shang & Liu (2026).[5]
- Fossil algae with morphological similarities to Proterozoic and Cambrian vendotaenids are reported from the Ordovician Landeyran Formation (France) by Vayda, Birolini & Xiao (2026).[6]
- Jeon et al. (2026) study the growth characteristics of Palaeoaplysina from the Permian (Asselian) strata of the Tyrrellfjellet Member of the Wordiekammen Formation (Svalbard, Norway), and interpret Palaeoaplysina as more likely to be an alga (probably a red alga) than a sponge or cnidarian.[7]
- Zhao et al. (2026) link the displacement of green eukaryotic algae by phytoplankton groups whose plastids are derived from rhodophytes as the dominant marine phytoplankton in the early Mesozoic to structural characteristics of red lineage phytoplankton that enhanced their resistance to environmental reactive oxygen species.[8]
- Evidence of changes of cellular structure of coralline algae from Meghalaya (northeast India) in response to environmental changes during the Paleocene–Eocene thermal maximum, resulting in the studied algae maintaining calcification in spite of high temperatures and acidification of surface waters, is presented by Melbourne, Sarkar & Schmidt (2026).[9]
- A study on the anatomy and diversity in organization of Pachytheca from the Silurian and Devonian strata from Welsh Borderland (United Kingdom), interpreted as an organism of uncertain phylogenetic placement with most likely affinities with green algae, is published by Edwards et al. (2026).[10]
- Iturain, Martínez & Olivera (2026) reconstruct the life cycle of Jurassic tasmanitid prasinophytes from the Los Molles Formation (Argentina).[11]
Non-vascular plants
Bryophyta
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Kimmerera[12] |
Gen. et sp. nov |
Walker et al. |
Late Cretaceous (Campanian) |
Antarctica |
A member of Bryopsida of uncertain affinities. The type species is K. cyanifera. |
||||
|
Meteoriella parvicella[13] |
Sp. nov |
Valid |
Wolski, Kaczmarek & Ignatov |
Eocene |
Europe (Baltic Sea region) |
A moss belonging to the family Hylocomiaceae. |
|||
Marchantiophyta
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Dinckleria opaca[14] |
Sp. nov |
Renner & Paulsen |
Eocene |
Anglesea amber |
A liverwort, a species of Dinckleria. |
||||
|
Frullania tseltal[15] |
Sp. nov |
Juárez-Martínez et al. |
Miocene |
A liverwort, a species of Frullania. |
|||||
|
Frullania tsotsil[15] |
Sp. nov |
Juárez-Martínez & Estrada-Ruiz in Juárez-Martínez et al. |
Miocene |
Mexican amber |
A liverwort, a species of Frullania. |
||||
|
Marchesinia pauchi[16] |
Sp. nov |
Valid |
Juárez-Martínez, Gradstein & Estrada-Ruiz in Juárez-Martínez et al. |
Miocene |
Simojovel Formation |
||||
|
Sp. nov |
Horcajada-Tejero, Blanco-Moreno & Martín-Abad |
Early Cretaceous (Barremian) |
A liverwort belonging to the family Metzgeriaceae. |
||||||
Non-vascular plant research
- Evidence from the study of moss fossil from north-eastern European Russia, indicative of evolution of leaf developmental pathway in Permian protosphagnacean mosses similar to that of extant Sphagnum, is presented by Ignatov et al. (2026).[18]
- Tremblay & Mercadal (2026) interpret the dark cells preserved in Paleozoic liverwort fossils as homologous with oil body cells of extant liverwort.[19]
Lycophytes
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Nowenia[20] |
Gen. et sp. nov |
El-Abdallah & Tomescu in El-Abdallah et al. |
Devonian |
A zosterophyll. The type species is N. matsunagae. |
|||||
|
Selaginellites huatingensis[21] |
Sp. nov |
Song & Ding in Song et al. |
Middle Jurassic |
A member of Selaginellales. |
|||||
|
Sinostigmaria[22] |
Gen. et sp. nov |
Yang et al. |
Carboniferous (Viséan) |
Xiangbai Formation |
A member of Isoetales. Genus includes new species S. yisis. |
||||
Lycophyte research
- D'Antonio et al. (2026) report evidence of preservation of internal three-dimensional structure in specimens of Stigmaria from the Carboniferous strata in Illinois, Indiana and Iowa (United States), and evidence of differences between the rooting systems of Stigmaria and other rhizomorphic lycopsids, indicating that the studied structures likely are not homologous.[23]
- Xu et al. (2026) report evidence from morphology and stable isotope analysis from Permian–Triassic transitional lycophytes from southwest China interpreted as consistent with use of crassulacean acid metabolism photosynthesis similar to the one seen in extant Isoetales, and interpret the physiology of the studied lycophytes as a possible factor enabling their survival during the Permian–Triassic extinction event and subsequent recovery.[24]
- Peng et al. (2026) interpret Lycostrobus scottii as a member of Pleuromeiaceae on the basis of the study of fossil material from the Lower Jurassic (Hettangian) strata from Sweden; the authors also study the phylogenetic relationships of Devonian to Jurassic lycopsids and reconstruct the distribution of pleuromeian lycopsids during the Triassic-Jurassic transition, reporting evidence of their short-lived proliferation in pioneer communities in the aftermath of collapse of forest ecosystems at the end of the Triassic.[25]
Ferns and fern allies
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Lophosoria myanmarica[26] |
Sp. nov |
Li in Li et al. |
Late Cretaceous (Cenomanian) |
Kachin amber |
A species of Lophosoria. |
||||
|
Loxsomopsis minor[27] |
Sp. nov |
Li in Li, Li & Ma |
Late Cretaceous (Cenomanian) |
Kachin amber |
A species of Loxsomopsis. |
||||
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Cyathocarpus felicianoi[28] |
Sp. nov |
Correia, Šimůnek & Pereira |
Carboniferous (Gzhelian) |
Douro Carboniferous Basin |
A member of Marattiales belonging to the family Psaroniaceae. |
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|
Danaeopsis huatingensis[29] |
Sp. nov |
Sun & Dengin Sun et al. |
Middle Triassic |
Tongchuan Formation |
A member of the family Marattiaceae. |
||||
|
Danaeopsis xunyiensis[29] |
Sp. nov |
Sun & Dengin Sun et al. |
Middle Triassic |
Tongchuan Formation |
A member of the family Marattiaceae. |
||||
|
Polymorphopteris mei[30] |
Sp. nov |
Li et al. |
Permian |
A marattialean fern frond |
|||||
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Todites holmesii[31] |
Sp. nov |
Early Triassic |
An osmundalean fern. |
||||||
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Sp. nov |
Wang, Tao, Zhang, Wang, & Shi in Wang et al. |
Cretaceous (Albian-Cenomanian) |
Kachin amber |
A polypodialean fern. |
|||||
|
Polystichum espinarensis[33] |
Sp. nov |
Valid |
Aliaga-Castillo et al. |
Pliocene |
A species of Polystichum. Published online in 2025; the final version of the article naming it was published in 2026. |
||||
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Salvinia dashtensis[34] |
Sp. nov |
Valid |
Spagnuolo in Spagnuolo et al. |
Eocene |
Ghazij Formation |
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Other fern allies
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Keraphyton talentii[35] |
Sp. nov |
Champreux, Meyer-Berthaud & Decombeix |
Devonian (Famennian) |
Mandowa Mudstone Formation |
A member of Iridopteridales. |
||||
|
Paradoxopteris huertasii[36] |
Sp. nov |
Valid |
Palma-Castro et al. |
Early Cretaceous (Aptian) |
A paradoxopterid polypodiopsid fern of uncertain affinities. |
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Pteridological research
- Hollaar et al. (2026) report palynological evidence from strata from the Triassic-Jurassic transition in Europe interpreted as indicative of spread of fern-dominated savannas after forest collapse during the Triassic–Jurassic extinction, and of continental-scale fires of these savannas.[37]
- A study on changes of distribution and on the evolutionary history of members of the genera Equisetites and Neocalamites in Europe, Central Asia and Siberia during the Early and Middle Jurassic is published by Frolov & Mashchuk (2026).[38]
Conifers
Cheirolepidiaceae
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Arkansia axsmithii[39] |
Sp. nov |
Andruchow-Colombo & Matsunaga |
Early Cretaceous |
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|
Sp. nov |
Wei et al. |
Early Jurassic |
Fu'xian Formation |
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|
Classostrobus amealensis[41] |
Sp. nov |
Tekleva et al. |
Early Cretaceous (Hauterivian) |
||||||
|
Pseudofrenelopsis axsmithii[39] |
Sp. nov |
Andruchow-Colombo & Matsunaga |
Early Cretaceous |
Holly Creek Formation |
|||||
|
Pseudofrenelopsis pingliangensis[42] |
Sp. nov |
Lou & Ding in Lou et al. |
Early Cretaceous (Albian) |
Madongshan Formation |
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Cupressaceae
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Austrohamia vitrea[43] |
Sp. nov |
Molano et al. |
Jurassic |
A member of Cupressaceae sensu lato. |
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|
Cascadiastrobus[44] |
Gen. et sp. nov |
Dostal, Stockey & Rothwell |
Eocene |
A seed cone of a member of Cupressaceae. Genus includes new species C. beardii. |
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|
Cupressinoxylon marquesii[45] |
Sp. nov |
Nhamutole & Bamford |
Permian |
Matinde Formation |
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|
Kamikistrobus[46] |
Gen. et sp. nov |
Jiang & Yamada |
Late Cretaceous (Turonian) |
A member of the subfamily Taxodioideae. Genus includes new species K. primulus. |
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|
Sequoia primaria[47] |
Comb. nov |
(Miki) |
Miocene |
Tokiguchi Porcelain Clay Formation |
Moved from Sequoiadendron primarium Miki (1965). |
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|
Thuja lingbaoensis[48] |
Sp. nov |
Wang in Wang et al. |
Eocene |
Xiangcheng Formation |
A species of Thuja. |
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Pinaceae
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Pinus izberdana[49] |
Sp. nov |
Nosova in Nosova, Melnikov & Chumanova |
Late Cretaceous (Santonian-Campanian) |
A pine. |
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|
Schizolepidopsis gerrienneii[50] |
Sp. nov |
De Brito et al. |
Early Jurassic |
A member or a relative of the family Pinaceae. |
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|
Tsuga zhuoziensis[51] |
Sp. nov |
Valid |
Xiao et al. |
Miocene |
Hannuoba Formation |
A species of Tsuga. Announced online in 2025; the final version of the article naming it was published in 2026. |
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Podocarpaceae
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Circoporoxylon bighornense[52] |
Sp. nov |
Valid |
Hoff & Gee in Hoff, Gee & Storrs |
Late Jurassic |
|||||
|
Podocarpoxylon paralambertii[53] |
Sp. nov |
Valid |
Ramos, Brea & Kröhling |
Pleistocene |
El Palmar Formation |
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Taxaceae
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Torreya albertensis[54] |
Sp. nov |
Halbwidl, Seyfullah & West |
Late Cretaceous |
A species of Torreya. |
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Other conifers
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Lindleycladus changtuensis[55] |
Sp. nov |
Yu & Liang in Yu et al. |
Early Cretaceous (Aptian) |
Shahezi Formation |
A member of the family Podozamitaceae. |
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|
Prototaxoxylon sanpedrense[56] |
Sp. nov |
Siegloch et al. |
Late Triassic (Norian-Rhaetian) |
Mata Sequence of the Santa Maria Supersequence |
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|
Texoxylon[57] |
Gen. et sp. nov |
Singleton & Costanza |
Carboniferous (Kasimovian) |
A member of Coniferopsida of uncertain affinities. Genus includes new species T. fambroensis. |
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Conifer research
- Evidence of links between decline of Tsuga canadensis in North America and regional effects of climate changes during the Holocene is presented by Shuman (2026).[58]
- Zhou et al. (2026) reconstruct the general morphology of Pagiophyllum maculosum on the basis of the study of the first fossil material reported from the Lower Jurassic strata in China.[59]
- Evidence from the study of the Cenozoic fossil record of Metasequoia, indicative of southward shift of its distribution during the Neogene in response to global aridification and subsequent contraction of its range in response to climate changes during the Pleistocene, is presented by Chen et al. (2026).[60]
- Taxonomic revision of coniferous woods from the Oligocene strata of the Petroșani Basin (Romania) is published by Călin, Popa & Pirnea (2026).[61]
Bennettitales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Bugdaevaea[62] |
Gen. et sp. nov |
Valid |
Bickner et al. |
Early Cretaceous |
Tevshiingovi Formation |
A fossil seed attributable to the Bennettitales-Erdtmanithecales-Gnetales group. Genus includes new species B. lignitica. |
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|
Marythodaya[63] |
Nom. nov |
Valid |
Deshmukh |
Early Cretaceous (Albian) |
A seed plant belonging to the informal grouping Bennettitales-Erdtmanithecales-Gnetales; a replacement name for Thodaya Friis, Crane & Pedersen (2019). |
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|
Sp. nov |
Zhang & Xin in Zhang et al. |
Middle Jurassic (Aalenian–Bajocian) |
Yaojie Formation |
||||||
|
Sp. nov |
Wang, Tan, Zhang & Sun in Wang et al. |
Early Cretaceous |
Binggou Formation |
||||||
|
Sp. nov |
Zhang & Xin in Zhang et al. |
Middle Jurassic (Aalenian–Bajocian) |
Yaojie Formation |
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|
Nosovaea[62] |
Gen. et sp. nov |
Valid |
Bickner et al. |
Early Cretaceous |
A fossil seed attributable to the Bennettitales-Erdtmanithecales-Gnetales group. Genus includes new species N. striata. |
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|
Sp. nov |
Early Triassic |
||||||||
|
Sp. nov |
Morales-Toledo, Zepeda-Martínez & Cevallos-Ferriz |
Middle Jurassic (Bathonian–Callovian) |
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Bennettitalean research
- Villalva & Gnaedinger (2026) report the discovery of bennettitopsid and gnetopsid reproductive organs from the Upper Triassic strata of the Laguna Colorada Formation (Argentina).[68]
- Xu et al. (2026) revise the cuticle structures of Pterophyllum crassinervum and confirms its taxonomic validity.[69]
Flowering plants
Magnoliids
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Extroparvum[70] |
Gen. et sp. nov |
Tang, Matsunaga & Atkinson |
Late Cretaceous (Coniacian) |
A member of the family Lauraceae. The type species is E. occidentale. |
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|
Fissistigma jarwaense[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced (under the name "Melodorum jarwaense") by Tripathi, Pandey & Prasad (2002); validated in 2026. |
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|
Maasia palaeosumatrana[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced (under the name "Polyalthia palaeosumatrana") by Tripathi, Pandey & Prasad (2002); validated in 2026. |
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|
Miliusa miovelutina[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Tripathi, Pandey & Prasad (2002); validated in 2026. |
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|
Phoebe himachalensis[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Pandey et al. (2023); validated in 2026. |
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|
Trimeriantha[72] |
Gen. et sp. nov |
Wu et al. |
Late Cretaceous (Turonian-Santonian) |
Klikov Formation |
A member of Piperales. The type species is T. monopolyada. |
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Magnoliid research
- Rubalcava-Knoth et al. (2026) identify leaf architecture characters that can be used for identification of fossil members of Lauraceae at the family level.[73]
Monocots
Alismatales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Anomacolocasioides[74] |
Gen. et sp. nov |
Gieser, Donovan & Herrera in Gieser et al. |
Eocene |
A member of the family Araceae. Genus includes new species A. demkovichorum. |
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|
Eospirodela[75] |
Gen. et sp. nov |
Ali, Almeida & Khan in Ali et al. |
Eocene |
Palana Formation |
A member of the family Araceae. The type species is E. indica. |
||||
|
Gigantosagittata[74] |
Gen. et sp. nov |
Gieser, Donovan & Herrera in Gieser et al. |
Eocene |
Green River Formation |
A member of the family Araceae. Genus includes new species G. graingeriana. |
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Arecales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Sp. nov |
Vera et al. |
Late Cretaceous (Maastrichtian) |
A fossil palm stem. |
||||||
|
Sp. nov |
Kumar et al. |
Cretaceous-Paleocene transition |
A fossil palm stem. |
||||||
|
Sp. nov |
Vera et al. |
Late Cretaceous (Maastrichtian) |
Chorrillo Formation |
A fossil palm stem. |
|||||
|
Sp. nov |
Biswas et al. |
Miocene-Pliocene |
Tipam Group |
A fossil palm stem. |
|||||
|
Sp. nov |
Kumar et al. |
Cretaceous-Paleocene transition |
Deccan Intertrappean Beds |
A fossil palm stem. |
|||||
|
Sp. nov |
Kumar et al. |
Cretaceous-Paleocene transition |
Deccan Intertrappean Beds |
A fossil palm stem. |
|||||
|
Sp. nov |
Kumar & Khan |
Cretaceous-Paleocene transition |
Deccan Intertrappean Beds |
A pinnate palm leaf. |
|||||
|
Pindocarpon[80] |
Gen. et sp. nov |
Muci, Passalia & Iglesias |
Miocene |
A fossil palm fruit. The type species is P. chichinalensis. |
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Zingiberales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Alpinia siwalica[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Prasad, Ghosh & Tripathi (2004); validated in 2026. |
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|
Paleozingiberum[81] |
Gen. et sp. nov |
Chandra, Shukla & Shukla |
Paleogene |
Genus includes new species P. gurhanensis. |
|||||
Monocot research
- Evidence from the study of the fossil record of seagrasses, indicative of links between the biogeographical distribution of seagrasses throughout the evolutionary history of the group and long-term climate fluctuations, is presented by Tuya et al. (2026).[82]
- Redescription and a study on the affinities of Graminocarpon is published by Manchester et al. (2026), who interpret the studied plant as a possible member or relative of Arecaceae.[83]
- Bellot et al. (2026) reconstruct the evolutionary history of palms on the basis of phylogeny of extant members of the group determined from data from nuclear genes and on the basis of the study of the fossil record of the group.[84]
- Redescription and a study on the affinities of Palmoxylon santarosense, P. rionegrense and P. valchetense from the Allen Formation (Argentina) is published by Vera (2026).[85]
- Kumar et al. (2026) identify fossil material of Callistemonites from the Deccan Intertrappean Beds (India) as rachillae of members of Arecaceae.[86]
Basal eudicots
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Appianocarpa[87] |
Gen. et sp. nov |
Valid |
Rico et al. |
Eocene |
A member of the family Menispermaceae. Genus includes new species A. canadense. Announced in 2025; the final version of the article naming it was published in 2026. |
||||
|
Buxus winterscheidii[88] |
Sp. nov |
Sachse in Sachse & Wappler |
Miocene |
||||||
|
Platanus orientalifolia[89] |
Sp. nov |
Zhu & Jia in Jia et al. |
Eocene |
Xiangcheng Formation |
A species of Platanus. |
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Superasterids
Cornales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Davidia indica[90] |
Sp. nov |
Valid |
Ali, Su & Khan in Ali et al. |
Eocene |
A species of Davidia. Published online in 2025; the final version of the article naming it was published in 2026. |
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Ericales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Ardisia siwalika[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Prasad et al. (2025); validated in 2026. |
||||
|
Herendeeniodoxa[91] |
Gen. et sp. nov |
Valid |
Pigg et al. |
Paleocene |
A member of the family Actinidiaceae. Genus includes new species H. willistonensis. |
||||
|
Sarcosperma mioarboreum[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Prasad, Ghosh & Tripathi (2004); validated in 2026. |
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Gentianales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Aganosmophyllum[92] |
Gen. et sp. nov |
Bhatia & Srivastava in Bhatia, Adhikari & Srivastava |
Paleocene |
Tura Formation |
A member of the family Apocynaceae. The type species is A. nongalbibraensis. |
||||
Icacinales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Goweria bacatana[93] |
Sp. nov |
Puente-Santos & Carvalho in Puente-Santos et al. |
Paleocene |
A member of the family Icacinaceae. |
|||||
|
Mappia siwalika[94] |
Sp. nov |
Valid |
Prasad et al. |
Miocene |
A species of Mappia. |
||||
|
Palaeophytocrene paramoae[93] |
Sp. nov |
Puente-Santos & Carvalho in Puente-Santos et al. |
Paleocene |
Bogotá Formation |
A member of the family Icacinaceae. |
||||
|
Punctiuga[93] |
Gen. et sp. nov |
Puente-Santos & Carvalho in Puente-Santos et al. |
Paleocene |
Bogotá Formation |
A member of the family Icacinaceae. The type species is P. bachue. |
||||
Lamiales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Fraxinoxylon sihongense[95] |
Sp. nov |
Zhu, Li & Cheng in Zhu et al. |
Miocene |
Xiacaowan Formation |
A member of the family Oleaceae. |
||||
Solanales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Albionites[96] |
Gen. et comb. nov |
Deanna & Knapp in Deanna et al. |
Eocene |
Poole Formation |
A member of the family Solanaceae; a new genus for "Solanum" arnense Chandler (1962). |
||||
|
Hyoscyamosperma[96] |
Gen. et 2 sp. nov |
Deanna & Smith in Deanna et al. |
Oligocene to Quaternary |
A member of the family Solanaceae. The type species is H. daturoides; genus also includes H. undulatus. |
|||||
|
Seminuta[96] |
Gen. et sp. nov |
Deanna & Smith in Deanna et al. |
Pliocene to Pleistocene |
A member of the family Solanaceae. The type species is S. pliocenica. |
|||||
|
Sinuatitesta[96] |
Gen. et comb. nov |
Deanna & Knapp in Deanna et al. |
Oligocene to Pleistocene |
A member of the family Solanaceae; a new genus for "Solanum" foveolatum Negru (1986). |
|||||
|
Solanotes[96] |
Gen. et sp. nov |
Deanna & Smith in Deanna et al. |
Oligocene to Pleistocene |
A member of the family Solanaceae. The type species is S. dorofeevii. |
|||||
|
Solanum miocenicum[96] |
Sp. nov |
Deanna & Smith in Deanna et al. |
Oligocene to Pleistocene |
A species of Solanum. |
|||||
|
Thanatosperma[96] |
Gen. et sp. nov |
Deanna & Knapp in Deanna et al. |
Pliocene to Holocene |
A member of the family Solanaceae. The type species is T. minutum. |
|||||
Superasterid research
- Lu et al. (2026) study the fossil material of Nyssa sibirica from the Pliocene strata from the Yuxi Basin (Yunnan, China) and reconstruct the geographic distribution of tupelos throughout their evolutionary history, interpreting the species belonging to this genus as originating in warm and humid environments, with their distribution contracting as a result of climate cooling during the Neogene.[97]
- González-Ramírez, Deanna & Smith (2026) reconstruct the evolutionary history of Solanaceae on the basis of data from extant and fossil taxa, reporting evidence of Late Cretaceous origin of the group.[98]
Superrosids
Fabales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Adinobotrys kathgodamensis[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced (under the name "Millettia kathgodamensis") by Prasad, Ghosh & Tripathi (2004); validated in 2026. |
||||
|
Derris prakashii[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Prasad, Ghosh & Tripathi (2004); validated in 2026. |
||||
|
Entada awasthii[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Chor Khola Formation |
Leaf fossil originally described under the name "Entada palaeoscandens" by Awasthi & Prasad (1990). |
|||
|
Entada miophaseoloides[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Surai Khola Formation |
Seeds originally described under the name "Entada palaeoscandens" by Awasthi & Prasad (1990). |
|||
|
Pahudioxylon pakistanicum[99] |
Sp. nov |
Izhar, Su & Oskolski in Izhar et al. |
Miocene |
Kamlial Formation |
A member of the family Fabaceae belonging to the subfamily Detarioideae. |
||||
|
Parvileguminophyllum deperdita[100] |
Comb. nov |
Valid |
(Saporta) |
Oligocene and Miocene |
Moved from Mimosa deperdita Saporta (1861) |
||||
|
Parvileguminophyllum norica[100] |
Comb. nov |
Valid |
(Unger) |
Eocene and Oligocene |
Moved from Caesalpinia norica Unger (1850). |
||||
|
Parvileguminophyllum oblita[100] |
Comb. nov |
Valid |
(Saporta) |
Oligocene |
Moved from Acacia oblita Saporta (1889) |
||||
|
Gen. et sp. nov |
Hernández-Damián et al. |
Miocene |
La Quinta Formation |
A member of the family Fabaceae belonging to the tribe Mimoseae. The type species is S. mijangosii. |
|||||
|
Spatholobus zhurongii[102] |
Sp. nov |
Zhao & Xie in Zhao et al. |
Miocene |
Bangmai Formation |
A species of Spatholobus. |
||||
Fagales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Gen. et sp. nov |
Valid |
Manchester et al. |
Paleocene |
A member of the family Fagaceae. Genus includes new species H. nixonii. Published online in 2025; the final version of the article naming it was published in 2026. |
|||||
|
Quercus bernardii[104] |
Sp. nov |
Valid |
Denk, van Zuijlen & Krings |
Miocene |
An oak. |
||||
|
Quercus liensis[105] |
Sp. nov |
Thongsangtum, Huang & Su & Thongsangtum et al. |
Oligocene–Miocene |
Li Formation |
An oak. |
||||
Malpighiales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Antidesma prasadii[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Churia Formation |
Announced (under the name "Antidesma miocenicum") by Prasad & Dwivedi (2007); validated in 2026. |
|||
|
Antidesma sarkaghatense[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced (under the name "Antidesma miocenicum") by Tiwari et al. (2022); validated in 2026. |
||||
|
Eogarcinia[106] |
Gen. et sp. nov |
Valid |
Ali, Almeida & Khan in Ali et al. |
Eocene |
Fossil flowers with affinities with Garcinia. Genus includes new species E. longistaminata. Published online in 2025; the final version of the article naming it was published in 2026. |
||||
|
Parasalicaceoxylon[107] |
Gen. et sp. nov |
Hung & Oskolski in Hung et al. |
Eocene |
Na Duong Formation |
A member of the family Salicaceae. The type species is P. naduongensis. |
||||
|
Rhizophoreaefolium[108] |
Gen. et sp. nov |
Carpenter et al. |
Eocene |
A member of the family Rhizophoraceae. Genus includes new species R. pirukwimukati. |
|||||
|
Salicoxylon meridionale[109] |
Sp. nov |
Pujana et al. |
Oligocene–Miocene |
Río Guillermo Formation |
Fossil wood of a member of the family Salicaceae. |
||||
|
Scolopia himachalensis[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Prasad et al. (2025); validated in 2026. |
||||
|
Tetrapterys miocenica[110] |
Comb. nov |
Valid |
(Berry) |
Miocene |
A species of Tetrapterys; moved from Gyrocarpus miocenica Berry (1937). |
||||
Malvales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Ayenia zhangpuensis[111] |
Sp. nov |
Wu et al. |
Miocene |
Zhangpu amber |
|||||
|
Dryobalanops rajangensis[112] |
Sp. nov |
Othman et al. |
Miocene |
Merit-Pila Formation |
A species of Dryobalanops. |
||||
|
Malvaciphyllum checuorum[113] |
Sp. nov |
Valid |
Puente-Santos & Carvalho in Puente-Santos, Carvalho & Herrera |
Paleocene |
A member of the family Malvaceae. |
||||
|
Pachira kathgodamica[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced (under the name "Pachira palaeomalabarica") by Prasad, Ghosh & Tripathi (2004); validated in 2026. |
||||
|
Tilia pentagona[114] |
Sp. nov |
Chen, Jia & Xing in Chen et al. |
Miocene |
A species of Tilia. |
|||||
|
Tilia perpendicularis[114] |
Sp. nov |
Chen et al. |
Miocene |
Duho Formation |
A species of Tilia. |
||||
|
Umarsaria[115] |
Gen. et sp. nov |
Singh et al. |
Eocene |
Umarsar lignite |
A flower of malvaceous affinity. Genus includes new species U. asahnii. |
||||
Myrtales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Capella[116] |
Gen. et sp. nov |
Rozefelds et al. |
Oligocene |
A member of Melastomataceae. Genus includes new species C. raulingsii. |
|||||
|
Lagerstroemia himachalensis[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Prasad, Singh & Singh (2025); validated in 2026. |
||||
|
Lagerstroemia jamraniensis[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Prasad, Ghosh & Tripathi (2004); validated in 2026. |
||||
|
Syzygium miocenicum[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Prasad & Prakash (1984); validated in 2026. |
||||
|
Syzygium paleosalicifolium[117] |
Sp. nov |
Sadanand, Bhatia & Srivastava in Sadanand et al. |
Miocene |
Kasauli Formation |
A species of Syzygium. |
||||
|
Terminalia miopaniculata[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Prasad et al. (2025); validated in 2026. |
||||
|
Trapa gokarnansis[118] |
Sp. nov |
Khatri in Khatri et al. |
Pleistocene |
A species of Trapa. |
|||||
Oxalidales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Eucryphia nirihuaensis[119] |
Sp. nov |
Passalia et al. |
Miocene |
Ñirihuau Formation |
A species of Eucryphia. |
||||
|
Eucryphia paraglutinosa[119] |
Sp. nov |
Passalia et al. |
Miocene |
Ñirihuau Formation |
A species of Eucryphia. |
||||
Rosales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Dryas nukabiraensis[120] |
Sp. nov |
Valid |
Narita & Oppata |
Miocene |
Tokachihoroka Formation |
||||
|
Ficus eodrupacea[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced (under the name "Ficus eomysorensis") by Tripathi, Pandey & Prasad (2002); validated in 2026. |
||||
|
Ficus prasadii[71] |
Nom. nov |
Valid |
Doweld & Saxena in Saxena, Doweld & Prasad |
Miocene |
A replacement name for Ficus nepalensis Prasad (1989). |
||||
|
Ziziphus prasadii[71] |
Nom. nov |
Valid |
Doweld & Saxena in Saxena, Doweld & Prasad |
Miocene |
A replacement name for Ziziphus miocenica Prasad (1994). |
||||
|
Ziziphus singhii[121] |
Nom. nov |
Valid |
Saxena & Doweld |
Miocene |
Dafla Formation |
A replacement name for Ziziphus indica Singh & Prakash (1980). |
|||
Sapindales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Arytera miolitoralis[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Churia Group |
Announced by Prasad et al. (2019); validated in 2026. |
|||
|
Arytera nepalensis[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Churia Group |
Announced by Prasad et al. (2019); validated in 2026. |
|||
|
Atalantia prasadii[71] |
Nom. nov |
Valid |
Doweld & Saxena in Saxena, Doweld & Prasad |
Miocene |
A replacement name for Atalantia miocenica Prasad (1994). |
||||
|
Baravalosphaera[122] |
Gen. et sp. nov |
Chen, Ersoy, Boura, Herrera & Del Rio in Ersoy et al. |
Oligocene |
A member of the family Anacardiaceae. Genus includes new species B. operculata. |
|||||
|
Canarium siwalicum[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced by Prasad, Singh & Singh (2025); validated in 2026. |
||||
|
Koelreuteria cyrtinervis[123] |
Sp. nov |
Xie & Jia in Xie et al. |
Eocene |
Huazhige Formation |
A species of Koelreuteria. |
||||
|
Koelreuteria quasibipinnata[123] |
Sp. nov |
Xie et al. |
Miocene |
A species of Koelreuteria. |
|||||
|
Koelreuteria truncatocarpa[123] |
Sp. nov |
Xie et al. |
Miocene |
A species of Koelreuteria. |
|||||
|
Lepidopetalum miocenicum[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Miocene |
Announced (under the name "Cupania miocenica") by Prasad, Ghosh & Tripathi (2004); validated in 2026. |
||||
|
Palaeochoerospondias[122] |
Gen. et comb. nov |
Ersoy, Chen, Boura, Herrera & Del Rio in Ersoy et al. |
Eocene and Oligocene |
A member of the family Anacardiaceae. |
|||||
|
Swietenia palaeomahagoni[71] |
Sp. nov |
Valid |
Saxena, Doweld & Prasad |
Paleocene-Eocene |
Palana Formation |
Announced by Chandra et al. (2023); validated in 2026. |
|||
|
Swintonia eocenica[124] |
Sp. nov |
Ali & Khan in Ali et al. |
Eocene |
Palana Formation |
|||||
|
Uintacarpa[125] |
Gen. et sp. nov |
Valid |
Manchester, Judd & Tiffney |
Eocene |
Green River Formation |
A Sapindalean fruit of uncertain affinity. |
|||
|
Zanthoxylum guipingense[126] |
Sp. nov |
Xu, Song & Jin in Xu et al. |
Miocene |
Erzitang Formation |
A species of Zanthoxylum. |
||||
Saxifragales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Trochodendroides cuneatum[127] |
Comb. nov |
Valid |
(Newberry) |
Paleocene |
A species of Trochodendroides; moved from Populus cuneata Newberry (1868). |
||||
|
Trochodendroides flexuosa[127] |
Comb. nov |
Valid |
(Hollick) |
Paleocene |
A species of Trochodendroides; moved from Populus flexuosa Hollick (1936). |
||||
|
Trochodendroides genesevianum[127] |
Comb. nov |
Valid |
(Chandrasekharam) |
Paleocene |
A species of Trochodendroides; moved from Cercidiphyllum genesevianum Chandrasekharam (1974). |
||||
Vitales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Austrovideira barivierae[128] |
Sp. nov |
Chen et al. |
Oligocene |
A member of the family Vitaceae. |
|||||
|
Leea himachalensis[94] |
Sp. nov |
Valid |
Prasad et al. |
Miocene |
A species of Leea. |
||||
|
Vitis praerotundifolia[128] |
Sp. nov |
Chen et al. |
Eocene and Oligocene |
Quercy Phosphorites Formation |
A species of Vitis. |
||||
|
Vitis quercyensis[128] |
Sp. nov |
Chen et al. |
Eocene |
Quercy Phosphorites Formation |
A species of Vitis. |
||||
Zygophyllales
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Larreoxylon[129] |
Gen. et sp. nov |
Franco et al. |
Miocene |
Mariño Formation |
A member of the family Zygophyllaceae belonging to the subfamily Larreoideae. Genus includes new species L. cuyensis. |
||||
Superrosid research
- Velasco-Flores et al. (2026) report the discovery of stem fossils of Euphorbia canariensis from the Pleistocene (Chibanian) strata of the Diego Hernández Formation (Tenerife, Canary Islands, Spain), preserved in their original distribution as a result of volcanic eruption, and representing the first record of fossils attributed to this species.[130]
- Lu et al. (2026) study the affinities of Albizia fossil leaflets from the Miocene strata from the Xiangyang Coal Mine (Yunnan, China), and interpret them as indicative of presence of ancestors of Albizia julibrissin in southwest China during or before the late Miocene.[131]
- Krejčíř et al. (2026) describe silicified oak wood (most closely resembling members of the genus Trigonobalanus) from the Menilite Formation (Czech Republic) associated with termite coprolites and microscopic fungal structures, and interpret the studied wood as consistent with presence of evergreen broad–leaved forests during the Oligocene.[132]
- Sobek et al. (2026) redescribe the type material of Fagus haidingeri.[133]
- Ali et al. (2026) report the discovery of fossil material of cf. Backhousia sp. from the Eocene strata of the Palana Formation (India), representing the first fossil record a member of this genus outside Australia.[134]
Other eudicots
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Doliofolium[135] |
Gen. et sp. nov |
Wilf, Giraldo & Carpenter in Wilf et al. |
Eocene |
Salt Creek Formation |
A member of the family Dilleniaceae. The type species is D. cooksoniae. |
||||
Other angiosperms
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Jixia jiuquanensis[136] |
Sp. nov |
Peng et al. |
Early Cretaceous |
A basal flowering plant. |
|||||
|
Kanalflorus[137] |
Gen. et sp. nov |
Valid |
Hernández-Damián et al. |
Late Cretaceous (Campanian) |
Angostura Formation |
A flowering plant of uncertain affinities, with a floral structure similar to those of eudicots, especially extant members of Apiales. Genus includes new species K. variabilis. |
|||
|
Kohlsia[138] |
Gen. et sp. nov |
Valid |
Manchester, Judd & Tiffney |
Eocene |
A herbaceous eudicot of uncertain affinities, possibly a superasterid. Genus includes new species K. parachutensis. |
||||
|
Quechu[139] |
Gen. et sp. nov |
Siegert & Gandolfo |
Eocene |
A fossil fruit of uncertain affinities. Genus includes new species Q. fratersuus. |
|||||
General angiosperm research
- Evidence from the study of the fossil record and molecular clock analysis, interpreted as indicative of Late Jurassic origin of flowering plants, is presented by Wu et al. (2026).[140]
- Evidence of early Albian age of the early angiosperm herbaceous assemblage from the Frentsevka Formation (Primorsky Krai, Russia) is presented by Golovneva et al. (2026).[141]
- Lee et al. (2026) report the discovery of a diverse assemblage of fossil diaspores from the Campanian strata of the Jose Creek Formation (McRae Group; New Mexico, United States), interpreted as indicative of evolution of diverse dispersal strategies of flowering plants during the Cretaceous.[142]
- Song et al. (2026) describe a flower of Tropidogyne cf. pentaptera from the Cretaceous amber from Myanmar preserved with four instead of five tepals, providing evidence of variability of floral organ number in mid-Cretaceous eudicots.[143]
Other plants
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Decaturospermum[144] |
Gen. et comb. nov |
Valid |
Manchester & Crane |
Late Cretaceous (Cenomanian) |
A possible member of Gnetales; a new genus for "Laurus" macrocarpus Lesquereux (1868). |
||||
|
Dengfengfructus[145] |
Gen. et sp. nov |
Wang et al. |
Permian |
Lower Shihezi Formation |
A fossil plant organ with similarities to flowering plant fruits. The type species is D. maxima. |
||||
|
Dopyeria[146] |
Gen. et sp. nov |
Valid |
Gensel |
Devonian (Emsian) |
A basal euphyllophyte. Genus includes new species D. elongata. |
||||
|
Gnetopsis villosa[147] |
Sp. nov |
Li & Xue in Li et al. |
Carboniferous |
Zhangshuwan Formation |
A member of Lagenospermopsida of uncertain affinities. |
||||
|
Hermanophyton knollii[148] |
Sp. nov |
Decombeix & Krings |
Late Cretaceous |
A putative gymnosperm. |
|||||
|
Ixostrobus bilobus[149] |
Sp. nov |
Chen, Zhang & Wang in Chen et al. |
Jurassic |
Male cones of members of Czekanowskiales. |
|||||
|
Neoparadoxa[63] |
Nom. nov |
Valid |
Deshmukh |
Middle Jurassic (Callovian) |
A gymnosperm with several morphological features formerly restricted to angiosperms; a replacement name for Paradoxa Liu, Shen & Wang (2023). |
||||
|
Panxia spinosa[150] |
Sp. nov |
Shen, Xue & Feng in Shen et al. |
Devonian |
Haikou Formation |
A member of Cladoxylopsida. |
||||
|
Paracycas pectinatus[151] |
Comb. nov |
(Berger) |
Triassic–Jurassic transition |
A cycad; moved from Cycadites pectinatus Berger (1832). |
|||||
|
Pseudotorellia yilongensis[152] |
Sp. nov |
Dong et al. |
Early Cretaceous |
Huolinhe Formation |
A ginkgophyte leaf. |
||||
|
Rellimia piedboeufii[153] |
Comb. nov |
(Kräusel & Weyland) |
Devonian |
A progymnosperm; moved from Protopteridium piedboeufii Kräusel & Weyland (1932). |
|||||
|
Shangyuania[154] |
Gen. et sp. nov |
Liu & Tian in Liu et al. |
Early Cretaceous |
A member of the family Ephedraceae. The type species is S. gracilis. |
|||||
|
Sp. nov |
Jiang & Xu in Xu et al. |
Devonian |
Hujiersite Formation |
A member of Aneurophytales. |
|||||
|
Sp. nov |
Anderson, Barboni & Rozefelds |
Triassic (Ladinian–Carnian) |
|||||||
Other plant research
- A study on the morphology of the stem apex of Medullosa stellata, interpreted as indicative of presence of a complex vascular system, as well as indicating that members of Medullosales differed in stem development from the majority of extant seed plants, is presented by Portailler & Luthardt (2026).[157]
- New fossil material of Pinnagigantonoclea guizhouensis, providing evidence of its creeping habit, is described from the Permian Upper Shihhotse/Shangshihezi Formation (Henan, China) by Li et al. (2026).[158]
- Pratt et al. (2026) synonymize Carboniferous taxa Cordaites grandifolius, Noeggerathia flabellata and Ginkgophyllum delvalii under the name Ginkgophytopsis flabellata.[159]
- Jiang et al. (2026) interpret the morphology of Fengweioxylon sinense as consistent with the interpretation of the studied plant as an evergreen tree with a 3–5 year leaf retention period, growing in environment with warm summer conditions, and interpret the morphology of corystosperms as consistent with their placement as intermediate between gymnosperms and flowering plants.[160]
- D'Rozario, Rößler & Yang (2026) describe ovules of members of Cardiocarpales from the Permian (Lopingian) strata of the Xuanwei Formation (Yunnan, China), preserved within the ground tissue of a Psaronius housuoensis and providing possible evidence of a close ecological relationship between the two plants.[161]
- Nosova & Zavialova (2026) provide new information on the anatomy of seeds of Allicospermum angrenicum from the Middle Jurassic Angren Formation (Uzbekistan), including evidence of preservation of pollen interpreted as suggestive of cycadalean affinities of the studied plant.[162]
- Jiang et al. (2026) use stomatal parameters and carbon isotope composition of cuticles of Ginkgoites and Czekanowskia from the Yanan Formation (China) to reconstruct CO2 concentrations, local temperature and elevation during the Aalenian, interpreted as consistent with the studied plants growing in a basin or low mountainous terrain with a warm, humid climate.[163]
- Zhao, Huang & Cai (2026) identify pollen diagnostic of Erdtmanithecales associated with Pelretes vivificus and members of the genus Parallelothrips from the Cretaceous amber from Myanmar, indicative of pollination of Cretaceous Erdtmanithecales by both thrips and kateretid beetles.[164]
- Zhao et al. (2026) report the discovery of kateretid and sap beetle specimens from the Cretaceous amber from Myanmar associated with dense aggregations of Eucommiidites pollen grains, interpreted as evidence of pollination of members of Erdtmanithecales by insects.[165]
Palynology
| Name | Novelty | Status | Authors | Age | Unit | Location | Synonymized taxa | Notes | Images |
|---|---|---|---|---|---|---|---|---|---|
|
Anapiculatisporites grossus[166] |
Sp. nov |
Gutiérrez et al. |
Permian |
A trilete spore. |
|||||
|
Antulsporites constrictus[167] |
Sp. nov |
Ruffo Rey, Balarino & Gutiérrez |
Middle Triassic |
Cerro de Las Cabras Formation |
A bryophyte spore. |
||||
|
Antulsporites incipiens[167] |
Sp. nov |
Ruffo Rey, Balarino & Gutiérrez |
Middle Triassic |
Cerro de Las Cabras Formation |
A bryophyte spore. |
||||
|
Antulsporites robustus[167] |
Sp. nov |
Ruffo Rey, Balarino & Gutiérrez |
Middle Triassic |
Cerro de Las Cabras Formation |
A bryophyte spore. |
||||
|
Bacutriletes reguralis[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Echitriletes conicus[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Erlansonisporites depauperatus[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Erlansonisporites junggarensis[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Flabellisporites sparsulus[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Floricorbispora[168] |
Gen. et sp. nov |
Valid |
Peng et al. |
Triassic |
A spore. Genus includes new species F. zhoui. |
||||
|
Henrisporites grandis[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Henrisporites karamayensis[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Henrisporites rarus[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Horstisporites papillatus[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Luntaispora granulatus[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Narkisporites coacorvatus[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Narkisporites junggarensis[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Narkisporites sparsus[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Ovalipollis namibiensis[166] |
Sp. nov |
Gutiérrez et al. |
Permian |
A bisaccate pollen grain. |
|||||
|
Striatriletes inflatus[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Striatriletes junggarensis[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Sverdrupollenites zavatierii[166] |
Sp. nov |
Gutiérrez et al. |
Permian |
A colpate pollen grain. |
|||||
|
Tarimispora radiorugosa[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Trileites bullosus[168] |
Sp. nov |
Valid |
Peng et al. |
Triassic |
|||||
|
Trypophobiacites[169] |
Gen. et sp. nov |
De Benedetti in De Benedetti et al. |
Late Cretaceous (Maastrichtian) |
A non-pollen palynomorph of uncertain affinities, with similarities to modern green algae Coelastrum. Genus includes new species T. chubutensis. |
|||||
|
Tuberculatosporites tricaricoi[166] |
Sp. nov |
Gutiérrez et al. |
Permian |
A monolete spore. |
|||||
Palynological research
- Bek et al. (2026) report evidence of distribution of early cryptospores and trilete spores in Ordovician and Silurian temperate zones with average temperatures similar to those of present-day tropical belt, and interpret their fossil record as suggestive of similar physiological thermal tolerance in early and extant plants.[170]
- Wellman et al. (2026) describe the Devonian spore assemblages from the Portilla and Candás formations (Spain), and interpret spores from the latter formation as indicative of presence of a flora dominated by arborescent archaeopteridaleans and aneurophytaleans.[171]
- Gutiérrez et al. (2026) study the composition of the first palynological assemblage recovered from the Permian (probably Lopingian) strata of the upper member of the La Golondrina Formation (Argentina), providing evidence of presence of a forest dominated by members of Glossopteridales, with undergrowth including ferns, sphenophytes, lycophytes and bryophytes.[172]
- Evidence from the study of the palynological record from the Jiyuan Basin in the southern part of the North China Plate, indicative of four distinct phases of terrestrial vegetation transition across the Carnian pluvial episode that were temporally linked with indicators of volcanic activity and were accompanied by climate changes, is presented by Zhang et al. (2026).[173]
- Sajjadi Hezaveh & Hashemi-Yazdi (2026) publish two studies on the composition of the plant assemblages from the Triassic (Rhaetian) strata of the Qadir Member of the Nayband Formation (Iran) as indicated by the composition of assemblages of spores and pollen, interpreted as indicative of affinities of the studied flora with both floras from northern Gondwana and with ones from southern Laurasia.[174][175]
- Vilas-Boas et al. (2026) study the composition of Late Triassic and Early Jurassic palynological assemblages from the Algarve and Lusitanian basins (Portugal), providing evidence of overall dominance of xerophytic plants across both basins, as well as evidence of links of studied assemblages with floras from the western Tethyan margin and North America, and report malformed sporomorphs interpreted as evidence of environmental impact of Central Atlantic magmatic province activity.[176]
- Rosin et al. (2026) study the composition of the palynological assemblages from the Westbury, Lilstock and Redcar Mudstone formations in the Cheshire Basin (United Kingdom), recording changes of composition of vegetation in response to environmental changes during the latest Triassic and Early Jurassic.[177]
- A study on spores and pollen grains from the Schandelah-1 core (Germany), providing evidence of increased occurrence of malformed pollen grains and shifts in the composition of the palynofloral assemblage indicative of ecological stress during the Toarcian hyperthermal event, is published by Galasso, Foster & van de Schootbrugge (2026).[178]
- Yang et al. (2026) report evidence from multiproxy analyses (including the study of palynological assemblages) of continental succession from the Junggar Basin (China) indicative of a shift from fern groundcover to conifer canopy during the Jenkyns Event and of recovery of ferns after the event, as well as indicative of a more humid climate with reduced monsoon seasonality that reduced wildfire activity during the Jenkyns Event.[179]
- Evidence from the study of palynological assemblages from the Qaidam Basin (China), indicative of vegetation changes during the Middle Jurassic linked to a shift from a humid to more arid climate that was related to reduced obliquity, is presented by Tang et al. (2026).[180]
- Evidence from the study of palynological assemblages from the Upper Jurassic strata from the Binalud Mountains (Iran), indicative of increase in the abundance and diversity of warm-adapted cheirolepid conifers over time in response to a regional warming, is presented by Kalanat (2026).[181]
- Hofmann et al. (2026) interpret Gemmatricolpites from the Lower Cretaceous Araripe Basin (Brazil) as likely to be pollen of representatives of an extinct lineage of Aquifoliales originating from northern Gondwana as subsequently reaching a cosmopolitan distribution until the Eocene.[182]
- Buratti et al. (2026) study the composition of palynological assemblages from the Gorgo a Cerbara section (Barremian–Aptian transition; Italy), and report evidence of presence of pollen Afropollis cf. jardinus representing one of the earliest records of flowering plants in the Tethyan realm.[183]
- Zhang et al. (2026) study the composition of palynological assemblages from the Jiufengshan Formation (Dayangshu Basin, China), and report evidence of increase of taxonomic richness of the flowering plants in the studied area during the Aptian.[184]
- Carvalho et al. (2026) reconstruct the composition of Aptian assemblages of spore-producing plants from the south Atlantic margin and their responses to environmental changes at the time of the opening of the southern Atlantic Ocean on the basis of the study of palynological assemblages from eight Brazilian sedimentary basins.[185]
- Evidence from the study of palynological assemblages from Codó and Itapecuru formations, indicative of changes of composition of plant assemblages in northeastern Brazil in response to climate and moisture variability during the late Aptian, is presented by Correia et al. (2026).[186]
- Lorente (2026) calculates the biomass of Cenomanian conifers in the eastern North America and the amount of their dispersed pollen on the basis of the study of the fossil record from the Arlington Archosaur Section (Woodbine Group; Texas, United States) and comparisons with extant conifers.[187]
- Evidence from the study of spores, pollen and microcharcoal abundances from Paleogene sediments from a hydrothermal vent crater in the North Atlantic Igneous Province on the Norwegian Margin and from other mid- and high latitude continental margins, indicative of rapid vegetation and soil disturbances in response to environmental changes at the onset of the Paleocene–Eocene thermal maximum resulting in widespread appearance of fern-dominated pioneer vegetation across mid- and high-latitude regions of the world, is presented by Nelissen et al. (2026).[188]
- Raynaud et al. (2026) reconstruct the composition of the Eocene plant assemblage from the embrithopod-bearing Bultu-Zile site (Meryemdere Formation; Turkey) on the basis of the study of the freshwater-deposited palynoflora from the site, and interpreted as indicative of a swamp-freshwater environment.[189]
- Barreda et al. (2026) study the composition of the palynological assemblage from the Río Pichileufú locality (Huitrera Formation, Argentina), providing evidence of presence of a middle Eocene flora dominated by gymnosperms and Nothofagaceae, and including fossil pollen representing the oldest record of the crown group of Barnadesioideae reported to date.[190]
- Moseri et al. (2026) reconstruct changes of vegetation in southwestern South Africa during the Oligocene-Miocene transition on the basis of palynological record from the Elandsfontyn Formation.[191]
- Evidence from the study of palynological assemblages from the Miocene El Chacay Formation (Argentina) indicative of increase in floral diversity during the early Burdigalian before the onset of the Middle Miocene Climatic Optimum is presented by Tapia et al. (2026).[192]
- Pound et al. (2026) study the Miocene (Serravallian) palynoflora from the Kenslow Member of the Brassington Formation (United Kingdom), interpreted as fossil record of plant growing in an area with an oceanic type climate with more rainfall during the summer than the winter (but with no pronounced dry season), and report evidence of impact of seasonal changes of availability of moisture on the composition of the studied Miocene forest.[193]
- Evidence from the study of the palynological assemblage from the Cessaniti site in southern Italy, indicative of presence of a taxonomically diverse and structurally complex mangrove forest during the Tortonian, is presented by Niccolini & Bertini (2026).[194]
- Li et al. (2026) report evidence from the study of the palynological record from the East China Sea continental shelf spanning the past 71,000 years indicative of presence of a cool, dry temperate grassland biome during the lowstand intervals (including the Last Glacial Maximum), as well as evidence of presence of an open-forest landscape during the milder conditions of the Marine Isotope Stage 3, and interpret their findings as supporting the interpretation of the exposed East China Sea continental shelf as a habitat facilitating the initial dispersal of early modern humans into East Asia.[195]
- Evidence from the study of pollen record from eastern Nanling Mountains, indicative of impact of climate changes (and, since the late Holocene, human activities) on the composition of vegetation in the studied area during the last 46,000 years, as well as of existence of cool and humid refugia in subtropical China during the Last Glacial Maximum, is presented by Quan et al. (2026).[196]
- Morley et al. (2026) reconstruct the distribution of spruce, poplar and willow in northern Alaska (United States) during the last 20,000 years on the basis of pollen preserved in lake cores, reporting evidence of decline of spruce presence in the region between 16,000 and 11,000 years ago, its persistence in a single locality during this time interval and subsequent recovery.[197]
General research
- Cai et al. (2026) report evidence of a shift in organic carbon to total phosphorus ratios in marine siliciclastic strata from approximately 455 million years ago, interpreted as likely linked to the spread of early land plants during the Ordovician.[198]
- Lu et al. (2026) review evidence of impact of successive phases of plant terrestrialization on global coal accumulation.[199]
- Cooper & Hetherington (2026) study the sporophytes of Aglaophyton majus, Rhynia gwynne-vaughanii, Trichopherophyton teuchansii and Asteroxylon mackiei from the Devonian Rhynie chert (United Kingdom), and find no evidence of presence of true phloem in early plants with xylem.[200]
- Evidence of widespread presence of diterpenoid-rich surface resins in cuticles of coal-forming plants from the Devonian (Givetian) strata of the Haikou and Hujiersite formations (China) is presented by Song et al. (2026).[201]
- The oldest amber reported to date, likely produced by non-seed plants but sharing chemical components comparable with coniferous ambers, is described from the Devonian (Givetian) strata of the Hujiersite Formation (Xinjiang, China) by Luo et al. (2026).[202]
- Meyer-Berthaud, Young & Decombeix (2026) document a new assemblage of Devonian (Frasnian) plants from the Hervey Group (New South Wales, Australia), similar in composition to Frasnian plant assemblages from south China.[203]
- Evidence from the study of Devonian megafossil plant localities from the Catskill Mountains in New York and Pennsylvania (United States), interpreted as indicative of mass extinction among plants during the Late Devonian mass extinction, is presented by Retallack & Guo (2026).[204]
- A study on the affinities of early gymnospermous seeds and their evolutionary history from the late Devonian to the late Permian is published by Bateman, Spencer & Hilton (2026).[205]
- A study on the composition of the Carboniferous (late Pennsylvanian) plant assemblage from the Scisti e Arenarie di Iano Formation (Italy), interpreted as indicative of humid conditions with episodic marine influence, is published by Foggetti et al. (2026).[206]
- Santos et al. (2026) study the composition of the Permian plant assemblage from the Costela Mine locality (Pedra de Fogo Formation, Brazil) dominated by callipterid peltasperms, interpreted as indicative of biogeographic links with early Permian plant assemblages from Euramerica, and report evidence of plant-arthropod interactions and plant disease in fossils from the studied assemblage.[207]
- Negri & Toledo (2026) review evidence of mutualistic relationships between insects and gymnosperms before the emergence of flowering plants.[208]
- A diverse assemblage of plant cuticles and spores, providing evidence of presence of conifers, members of Peltaspermales and lycophytes, is reported from the Permian (Kungurian) strata from the Gorl locality in the Athesian Volcanic District (Italy) by Delfosse-Allain et al. (2026).[209]
- Jalfin et al. (2026) study changes of taxonomic diversity and community structure of the riparian forest known from fossil from the La Golondrina Formation (Argentina) during the Permian, reporting evidence of peak diversity in the Guadalupian and major ecological disruption near the Guadalupian–Lopingian transition.[210]
- A study on gymnosperm wood preserved as charcoal from the Madygen Formation (Kyrgyzstan), providing evidence of wildfire in the studied area near the Ladinian–Carnian transition, is published by Spiekermann et al. (2026).[211]
- Review of the composition of the Late Triassic (Carnian) flora from the Cave del Predil/Raibl (Italy) is published by Slodownik, Branz & Kustatscher (2026).[212]
- Fang et al. (2026) report evidence of acid rains coinciding with the Central Atlantic magmatic province volcanism during the Triassic-Jurassic transition, as well as evidence of critical destruction of plant biomass in terrestrial basins during the Triassic–Jurassic extinction that was likely linked to acid rains.[213]
- Gou et al. (2026) reconstruct the structure of the canopy-forming tree assemblage from the gymnosperm-dominated Yiwu Jurassic Forest known from the Middle Jurassic strata of the Xishanyao Formation (Xinjiang, China), and report evidence of higher productivity of the studied forest compared to modern temperate conifer forests.[214]
- Foster et al. (2026) provide estimates of height and mass of giant trees preserved as fossil logs from the Morrison Formation (western United States), and interpret the presence of these trees in western North America during the Late Jurassic as suggestive of long-term climatic cyclicity including both periods of arid conditions and periods of humid ones.[215]
- Evidence from the study of fossil plants from the Lower Cretaceous Jinju Formation (South Korea), indicative of presence of a temperate intermontane savanna in the studied area during the Albian, is presented by Lee, Kim & Looy (2026).[216]
- Vršanský et al. (2026) interpret the composition of fossil assemblages of dictyopteran insects from Russia and Australia as indicative of presence of high-latitude forests with tall tree canopies during the Cretaceous.[217]
- A study on the composition of the Cenomanian plant assemblage from the strata of the Utrillas Group from the Algora area (Guadalajara, Spain) is published by Sender, Bueno-Cebollada & Pérez-García (2026).[218]
- A new, diverse plant assemblage, providing evidence of presence of a mixed angiosperm-conifer woodland ecosystem, is described from the Turonian–Coniacian strata of the Moreno Hill Formation (New Mexico, United States) by Cilliers et al. (2026).[219]
- Greenwood & Conran (2026) review the fossil record of Cenozoic plants from the Kati Thanda–Lake Eyre, Woomera and northern deserts region of South Australia.[220]
- Taxonomic revision of the Oligocene (Chattian) flora from the La Val fossil site (Spain) is published by Moreno-Domínguez et al. (2026).[221]
- A study on the composition of the early Miocene plant assemblages known from leaf material from West Akrocheiras (Lesvos Petrified Forest, Greece) is published by Liapi et al. (2026).[222]
- Stiles et al. (2026) reconstruct climate changes and vegetation in the Upper Magdalena River Valley region (Colombia) during the middle and late Miocene, reporting evidence of surface cooling that exceeded global estimates, as well as evidence of presence of closed-canopy forests with increasing vegetation density.[223]
- Schartman, Polissar & Strömberg (2026) reconstruct the development of savannas in northwest Africa during the Miocene, reporting evidence of development of a C3 grass-rich savanna during the middle Miocene, and its gradual replacement by the C4 savanna in the late Miocene.[224]
- A study on the composition of the Miocene (Serravallian) plant assemblage from the Wolf clay pit in Graz-Andritz (Styrian Basin; Austria), interpreted as indicative of temperate climate without a pronounced dry period during the year, is published by Denk et al. (2026).[225]
- Wang et al. (2026) reconstruct the plant-insect interactions in the late Miocene Tatsumi-toge biota on the basis of the study of damage of fossil plants from the Ningyo-toge Formation (Japan) and comparisons with modern relatives of insects from the studied biota, reporting evidence of predominance of generalist insects that might have been linked to the late Miocene cooling and related environmental changes, and evidence of ecological stability of the Tatsumi-toge biota.[226]
- Góis-Marques et al. (2026) describe lava tree moulds from the San Roque locality, representing the oldest plant fossils from Tenerife (Canary Islands) reported to date, and providing evidence of presence of a forest ecosystem on Tenerife during the Pliocene.[227]
- A new, diverse assemblage of Plio-Pleistocene plants is described from the Kon Tum Formation (Vietnam) by Wang et al. (2026).[228]
- Allaby et al. (2026) reconstruct the environment of the Southern River system in southern Doggerland on the basis of sedimentological and sedimentary ancient DNA, and report evidence of presence of temperate trees indicative of presence of northern refugia during the early Mesolithic.[229]
- Evidence from the study of the fossil flora from the Quaternary tufas of the western Potiguar Basin (Brazil), indicative of a shift from a humid tropical environment supporting a mesophytic forest to the modern Caatinga biome, is presented by Aureliano et al. (2026).[230]
- Evidence from the study of modern leaves from swamp and river margins, indicating that studies that use fossil leaves as paleoclimate proxy and do not take into account the reduction of size of leaves from the surface litter and buried litter might result in underestimation of precipitation, is presented by Brown et al. (2026).[231]
Deaths
- Eminent U.S. paleobotanist David Dilcher dies. Dilcher was a National Academy of Science member, twice a Guggenheim Fellow, and a past president of the Botanical Society of America.[232]
References
- 1 2 Bucur, I. I.; Masse, J.-P.; Frau, C.; Fenerci-Masse, M. (2026). "New insights on calcareous algae from lower Aptian Urgonian carbonates of SE France". Cretaceous Research. 184 106369. Bibcode:2026CrRes.18406369B. doi:10.1016/j.cretres.2026.106369.
- ↑ Siver, P.A. (2026). "Taxonomy and phylogeny of Forticellula wolfei gen. et sp. nov., (Fragilariophyceae), an Eocene diatom with a unique cingulum from the Horsefly fossil locality, British Columbia, Canada". Diatom Research: 1–14. doi:10.1080/0269249X.2026.2677556.
- ↑ Du, W.; Wang, X.; Wang, Y.; Uesugi, K.; Yasutake, M.; Komiya, T. (2026). "Three-dimensional reconstruction of Ediacaran Ceramiales (Rhodophyta) from the phosphorite Doushantuo Formation, South China". Scientific Reports. 16 (1) 9935. Bibcode:2026NatSR..16.9935D. doi:10.1038/s41598-026-42410-5. PMC 13021990. PMID 41792433.
- ↑ Mohammed, K. A.; Moore, K. R.; Newell, C. R.; Brenner, D. C.; Talgatbek, A.; Mustapayeva, S.; Mamanov, Y.; Viete, D. R.; Smith, E. F. (2026). "Carbonate U-PB geochronology establishes flask-shaped microfossils from the Dzhanytas Group of southern Kazakhstan as mid-Tonian and the oldest globally". PALAIOS. 41 (3): 162–172. Bibcode:2026Palai..41..162M. doi:10.2110/palo.2024.031.
- ↑ You, H.; Shang, X.; Liu, P. (2026). "Early Cambrian occurrence of multicellular algae Wengania: Survivors of the terminal Ediacaran Kotlinian Crisis". Precambrian Research. 437 108061. Bibcode:2026PreR..43708061Y. doi:10.1016/j.precamres.2026.108061.
- ↑ Vayda, P. J.; Birolini, E.; Xiao, S. (2026). "Ediacaran-type vendotaenid macroalgae in an Ordovician Lagerstätte". Lethaia. 59 (2): 1–17. doi:10.18261/let.59.2.14.
- ↑ Jeon, J.; Lee, H.; Lee, Y.; Lee, M.; Choh, S.-J. (2026). "Taxonomic position and palaeoecology of Palaeoaplysina: insights from the lower Permian (Asselian) of Svalbard". Palaeoworld. 35 (3) 201091. Bibcode:2026Palae..3501091J. doi:10.1016/j.palwor.2026.201091.
- ↑ Zhao, Y.; Tong, M.; Tian, L.; Luo, G.; Li, P.; Song, H.; Chen, Z.; Xie, S.; Kappler, A.; Yuan, S. (2026). "Reactive oxygen species drove red lineage phytoplankton to displace green lineage phytoplankton during the Mesozoic". Proceedings of the National Academy of Sciences of the United States of America. 123 (2) e2521306123. Bibcode:2026PNAS..12321306Z. doi:10.1073/pnas.2521306123. PMC 12799162. PMID 41512038.
- ↑ Melbourne, L. A.; Sarkar, S.; Schmidt, D. N. (2026). "Exploring structural integrity of coralline algae in response to the environmental changes associated with the PETM: a tale of functional resistance". Palaeontology. 69 (1) e70039. Bibcode:2026Palgy..6970039M. doi:10.1111/pala.70039.
- ↑ Edwards, D.; Channing, A.; Axe, L.; Padilla Maqueo Mendez, E. (2026). "The Nature and Affinities of the Enigmatic Silurian–Devonian Genus Pachytheca from Britain". Monographs of the Palaeontographical Society. 179 (673): 1–87. doi:10.1080/02693445.2025.2654935.
- ↑ Iturain, V. R.; Martínez, M. A.; Olivera, D. E. (2026). "Ontogenetic stages and taphonomic analysis of Jurassic tasmanitids: Linking Pleurozonaria picunensis Quattrocchio and Tasmanites (Newton) Eisenack from the Los Molles Formation, Neuquén Basin, Argentina". Review of Palaeobotany and Palynology. 352 105631. Bibcode:2026RPaPa.35205631I. doi:10.1016/j.revpalbo.2026.105631.
- ↑ Walker, Z.; Bippus, A. C.; Iglesias, A.; Smith, S. Y.; Atkinson, B. A. (2026). "Cretaceous moss–cyanobacteria association reveals trophic interactions in polar forests of Antarctica". New Phytologist. 251 (6) nph.71428. doi:10.1111/nph.71428. PMC 13491244. PMID 42469917.
- ↑ Wolski, G. J.; Kaczmarek, S.; Ignatov, M. (2026). "Meteoriella parvicella sp. nov. (Bryophyta, Hylocomiaceae)—the first species with forked costae from Baltic amber". Phytotaxa. 747 (2): 207–214. Bibcode:2026Phytx.747..207W. doi:10.11646/phytotaxa.747.2.6.
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- ↑ Allaby, R. G.; Ware, R.; Cribdon, R.; Hansford, T. A.; Kinnaird, T.; Hamilton, D.; Kistler, L.; Murgatroyd, P.; Bates, R.; Fitch, S.; Gaffney, V. (2026). "Early colonization before inundation consistent with northern glacial refugia in Southern Doggerland revealed by sedimentary ancient DNA". Proceedings of the National Academy of Sciences of the United States of America. 123 (11) e2508402123. Bibcode:2026PNAS..12308402A. doi:10.1073/pnas.2508402123. PMC 12994208. PMID 41805578.
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- ↑ Brown, M. A.; Royer, D. L.; Nazzaro, V.; Azevedo-Schmidt, L. (2026). "Leaf size and shape as a paleoclimate proxy: investigating taphonomic biases within species". PALAIOS. 41 (1): 48–57. Bibcode:2026Palai..41...48B. doi:10.2110/palo.2025.037.
- ↑ "David Leonard Dilcher". Legacy.com. Retrieved August 22, 2026.