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Palaeobotanical and genetic data highlight the vulnerability of Picea in peninsular Italy
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-04-21 DOI: 10.1016/j.revpalbo.2025.105360
Camilla Avanzi , Federico Di Rita , Fabrizio Michelangeli , Juan Ochando , Paolo Piovani , Giovanni Giuseppe Vendramin , Donatella Magri , Andrea Piotti
Rear edge populations might be of disproportionate importance for the adaptation of temperate forest tree species to climate change. The study of past demographic dynamics and their effects on extant genetic diversity are therefore keys to understand how to manage these potentially relevant forest genetic resources. Here we combine a comprehensive review of palaeobotanical evidence from peninsular Italy throughout the Quaternary with new genetic data for Picea abies, focusing on all known rear edge populations from the boundary zone between the Alps and the northern Apennines, to shed light on timing and modes of the fragmentation processes leading these populations close to extirpation. Our data show that Picea abies experienced a complex Quaternary history mirrored by a concomitantly complex genetic structure. The population in the southwestern Alps and the two populations living in the northwestern Apennines appear to be the last remnants of a much wider Pleistocene distribution. During the last glacial period and the postglacial they had distinct spatiotemporal dynamics. These peripheral populations are characterized by peculiar genetic features, a substantial pairwise genetic differentiation and general genetic impoverishment, with a ∼ 20% reduction of their allelic richness with respect to other Alpine populations.
These results collectively indicate that the southernmost Italian populations of Picea abies, still present in the northern Apennines and in the southwestern Alps, are extremely vulnerable to extirpation, as already was the case with populations that progressively disappeared from southern and central Italy in the Middle and Upper Pleistocene, respectively, and from the north-eastern Apennines during the late Holocene.
{"title":"Palaeobotanical and genetic data highlight the vulnerability of Picea in peninsular Italy","authors":"Camilla Avanzi ,&nbsp;Federico Di Rita ,&nbsp;Fabrizio Michelangeli ,&nbsp;Juan Ochando ,&nbsp;Paolo Piovani ,&nbsp;Giovanni Giuseppe Vendramin ,&nbsp;Donatella Magri ,&nbsp;Andrea Piotti","doi":"10.1016/j.revpalbo.2025.105360","DOIUrl":"10.1016/j.revpalbo.2025.105360","url":null,"abstract":"<div><div>Rear edge populations might be of disproportionate importance for the adaptation of temperate forest tree species to climate change. The study of past demographic dynamics and their effects on extant genetic diversity are therefore keys to understand how to manage these potentially relevant forest genetic resources. Here we combine a comprehensive review of palaeobotanical evidence from peninsular Italy throughout the Quaternary with new genetic data for <em>Picea abies</em>, focusing on all known rear edge populations from the boundary zone between the Alps and the northern Apennines, to shed light on timing and modes of the fragmentation processes leading these populations close to extirpation. Our data show that <em>Picea abies</em> experienced a complex Quaternary history mirrored by a concomitantly complex genetic structure. The population in the southwestern Alps and the two populations living in the northwestern Apennines appear to be the last remnants of a much wider Pleistocene distribution. During the last glacial period and the postglacial they had distinct spatiotemporal dynamics. These peripheral populations are characterized by peculiar genetic features, a substantial pairwise genetic differentiation and general genetic impoverishment, with a ∼<!--> <!-->20% reduction of their allelic richness with respect to other Alpine populations.</div><div>These results collectively indicate that the southernmost Italian populations of <em>Picea abies</em>, still present in the northern Apennines and in the southwestern Alps, are extremely vulnerable to extirpation, as already was the case with populations that progressively disappeared from southern and central Italy in the Middle and Upper Pleistocene, respectively, and from the north-eastern Apennines during the late Holocene.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"339 ","pages":"Article 105360"},"PeriodicalIF":1.7,"publicationDate":"2025-04-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143877174","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
A new species of Stutzeliastrobus (Cupressaceae) from the Early Cretaceous of the Guyang Basin, northern China, and its paleoenvironmental implications
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-04-21 DOI: 10.1016/j.revpalbo.2025.105353
Xiaohui Xu , Jiangxue Deng , Liuyin Yang , Yeming Zhao , Stephen McLoughlin
A cupressaceous conifer, Stutzeliastrobus araucarioides comb. nov. is described from the Lower Cretaceous Guyang Formation in the Guyang Basin, central Inner Mongolia, northern China. Stutzeliastrobus araucarioides is known based on well-preserved leafy shoots with attached ovuliferous cones, and is characterized by elongate ovuliferous cones with numerous helically arranged, flat cone-scale complexes. Each complex is composed of a fused bract and ovuliferous scale and bears two seeds on the proximal to middle region. Stutzeliastrobus araucarioides is most similar in gross morphology to extant Taiwania cryptomerioides, but differs by having many more bract-scale complexes per cone. The features of S. araucarioides confirm that Stutzeliastrobus is closely relared to Taiwania. The new material enriches the fossil record of Stutzeliastrobus and adds to knowledge of the diversity of early Cupressaceae from the Early Cretaceous. Associated fossils and sedimentary facies indicate that S. araucarioides occupied lacustrine-paludal environments that hosted a diverse range of conifers and ginkgoaleans.
{"title":"A new species of Stutzeliastrobus (Cupressaceae) from the Early Cretaceous of the Guyang Basin, northern China, and its paleoenvironmental implications","authors":"Xiaohui Xu ,&nbsp;Jiangxue Deng ,&nbsp;Liuyin Yang ,&nbsp;Yeming Zhao ,&nbsp;Stephen McLoughlin","doi":"10.1016/j.revpalbo.2025.105353","DOIUrl":"10.1016/j.revpalbo.2025.105353","url":null,"abstract":"<div><div>A cupressaceous conifer, <em>Stutzeliastrobus araucarioides</em> comb. nov. is described from the Lower Cretaceous Guyang Formation in the Guyang Basin, central Inner Mongolia, northern China. <em>Stutzeliastrobus araucarioides</em> is known based on well-preserved leafy shoots with attached ovuliferous cones, and is characterized by elongate ovuliferous cones with numerous helically arranged, flat cone-scale complexes. Each complex is composed of a fused bract and ovuliferous scale and bears two seeds on the proximal to middle region. <em>Stutzeliastrobus araucarioides</em> is most similar in gross morphology to extant <em>Taiwania cryptomerioides</em>, but differs by having many more bract-scale complexes per cone. The features of <em>S. araucarioides</em> confirm that <em>Stutzeliastrobus</em> is closely relared to <em>Taiwania</em>. The new material enriches the fossil record of <em>Stutzeliastrobus</em> and adds to knowledge of the diversity of early Cupressaceae from the Early Cretaceous. Associated fossils and sedimentary facies indicate that <em>S. araucarioides</em> occupied lacustrine-paludal environments that hosted a diverse range of conifers and ginkgoaleans.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"339 ","pages":"Article 105353"},"PeriodicalIF":1.7,"publicationDate":"2025-04-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143870564","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Epidermal anatomy of Pterophyllum ptilum (Cycadophyta: Bennettitales) from the Upper Triassic of Sichuan Province, Southwest China 中国西南部四川省上三叠统 Pterophyllum ptilum(苏铁纲:Bennettitales)的表皮解剖图
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-04-15 DOI: 10.1016/j.revpalbo.2025.105351
Weiyu Lu , Han Wu , Tao Zhao , Patrick Blomenkemper , Zhuo Feng
Pterophyllum ptilum Harris 1932 is a distinctive fossil plant species that occurred exclusively in the Late Triassic but in a broad geographic distribution ranging from North Europe to East Asia. Thus, this species has long been considered significant in stratigraphic correlation of non-marine sequences. However, previous studies of P. ptilum have been mostly focused on the morphological characteristics of its foliages, a complete biological feature, particularly the epidermal anatomy, remains poorly understood. Here, we show detailed epidermal anatomies of P. ptilum based on well-preserved cuticular specimens from the Upper Triassic of Sichuan Province, Southwest China. Pterophyllum ptilum is characterised by petiolate leaves with small lateral leaflets, which possess contracted bases and bicuspid apices with five to eight parallel veins and syndetocheilic type stomata. In the leaflets, the stomata are only present on the abaxial surface, whereas the stomata are present on both the abaxial and adaxial surfaces of the rachis. Both the adaxial and abaxial leaflet surfaces can be divided into costal and intercostal fields. The epidermal cells in the costal fields are elongated rectangular but shortened rectangular in the intercostal fields. The stomata are only present in the intercostal fields of the abaxial leaflet surface. On the rachis, the epidermal cells are all elongated rectangular and arranged tightly in vertical files. Based on a thorough comparison of fossil records and observation of extant cycads, we propose that the bicuspid leaflet apices of P. ptilum may resulted from herbivorous arthropod apical feeding damage. Fossil records reveal that P. ptilum were primarily preserved in coastal plain, deltaic, and tidal flat environments in the South China Block; the absence of papillae and hairs in the present specimens may suggest a relatively more humid local environment.
{"title":"Epidermal anatomy of Pterophyllum ptilum (Cycadophyta: Bennettitales) from the Upper Triassic of Sichuan Province, Southwest China","authors":"Weiyu Lu ,&nbsp;Han Wu ,&nbsp;Tao Zhao ,&nbsp;Patrick Blomenkemper ,&nbsp;Zhuo Feng","doi":"10.1016/j.revpalbo.2025.105351","DOIUrl":"10.1016/j.revpalbo.2025.105351","url":null,"abstract":"<div><div><em>Pterophyllum ptilum</em> Harris 1932 is a distinctive fossil plant species that occurred exclusively in the Late Triassic but in a broad geographic distribution ranging from North Europe to East Asia. Thus, this species has long been considered significant in stratigraphic correlation of non-marine sequences. However, previous studies of <em>P. ptilum</em> have been mostly focused on the morphological characteristics of its foliages, a complete biological feature, particularly the epidermal anatomy, remains poorly understood. Here, we show detailed epidermal anatomies of <em>P. ptilum</em> based on well-preserved cuticular specimens from the Upper Triassic of Sichuan Province, Southwest China. <em>Pterophyllum ptilum</em> is characterised by petiolate leaves with small lateral leaflets, which possess contracted bases and bicuspid apices with five to eight parallel veins and syndetocheilic type stomata. In the leaflets, the stomata are only present on the abaxial surface, whereas the stomata are present on both the abaxial and adaxial surfaces of the rachis. Both the adaxial and abaxial leaflet surfaces can be divided into costal and intercostal fields. The epidermal cells in the costal fields are elongated rectangular but shortened rectangular in the intercostal fields. The stomata are only present in the intercostal fields of the abaxial leaflet surface. On the rachis, the epidermal cells are all elongated rectangular and arranged tightly in vertical files. Based on a thorough comparison of fossil records and observation of extant cycads, we propose that the bicuspid leaflet apices of <em>P. ptilum</em> may resulted from herbivorous arthropod apical feeding damage. Fossil records reveal that <em>P. ptilum</em> were primarily preserved in coastal plain, deltaic, and tidal flat environments in the South China Block; the absence of papillae and hairs in the present specimens may suggest a relatively more humid local environment.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"339 ","pages":"Article 105351"},"PeriodicalIF":1.7,"publicationDate":"2025-04-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143851589","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Palynology of the Early Pleistocene Kalibiuk and Kaliglagah Formations at Bentasari, Central Java, Indonesia
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-04-15 DOI: 10.1016/j.revpalbo.2025.105352
Harsanti P. Morley , Robert J. Morley
The Kaliglagah Formation in Central Java, of early Pleistocene age, yields abundant vertebrate fossils that predate the oldest occurrences of Javanese Homo erectus. This formation, together with the underlying Kalibiuk Formation, outcrops in the neighbourhood of Bentasari village, 20 km to the west of the classic outcrops at Bumiayu, Central Java. A 100 m exposure of this section was studied for palynology and sequence biostratigraphy. The analysis suggests that the section studied comprised two transgressive-regressive deltaic packages which probably formed as a result of two 41 kyr obliquity-driven climate cycles. It indicates that the Kalibiuk Formation comprises lower delta plain and delta front sediments that formed part of a large delta which was dominated by mangroves of the family Rhizophoraceae as well as Sonneratia (Sonneratiaceae). The lowermost part of the Kaliglagah Formation also formed on the lower delta plain of this delta, but the vegetation consisted mainly of the mangrove fern Acrostichum (Pteridaceae), together with the mangrove palm Nypa and the climbing fern Stenochlaena palustris (Blechnaceae). The upper part of the studied section of the Kaliglagah Formation formed on the upper delta plain in an open freshwater swamp setting vegetated mainly with Jussiaea (Onagraceae), Pandanus (Pandanaceae), Hanguana (Hanguanaceae) and Polygonum (Polygonaceae). The terra firma vegetation during time of deposition of the succession consisted of grassy savanna in the lowlands, indicating a strongly seasonal climate, and montane forests with Podocarpaceae in the upper catchment. The swamp and terra firma vegetation succession are compared to that in Perning, East Java, and other Javanese hominid sites.
The Kalibiuk and lower part of the Kaliglagah Formation, and also the Pucangan Formation at the Perning Homo erectus site, yielded the age-restricted palynomorph Stenochlaenidites papuanus, the parent plant of which went extinct across Sunda during the early Pleistocene, emphasising the older age of these localities compared to other Javanese hominid sites, such as Sangiran and Trinil where this taxon is missing.
{"title":"Palynology of the Early Pleistocene Kalibiuk and Kaliglagah Formations at Bentasari, Central Java, Indonesia","authors":"Harsanti P. Morley ,&nbsp;Robert J. Morley","doi":"10.1016/j.revpalbo.2025.105352","DOIUrl":"10.1016/j.revpalbo.2025.105352","url":null,"abstract":"<div><div>The Kaliglagah Formation in Central Java, of early Pleistocene age, yields abundant vertebrate fossils that predate the oldest occurrences of Javanese <em>Homo erectus</em>. This formation, together with the underlying Kalibiuk Formation, outcrops in the neighbourhood of Bentasari village, 20 km to the west of the classic outcrops at Bumiayu, Central Java. A 100 m exposure of this section was studied for palynology and sequence biostratigraphy. The analysis suggests that the section studied comprised two transgressive-regressive deltaic packages which probably formed as a result of two 41 kyr obliquity-driven climate cycles. It indicates that the Kalibiuk Formation comprises lower delta plain and delta front sediments that formed part of a large delta which was dominated by mangroves of the family Rhizophoraceae as well as <em>Sonneratia</em> (Sonneratiaceae). The lowermost part of the Kaliglagah Formation also formed on the lower delta plain of this delta, but the vegetation consisted mainly of the mangrove fern <em>Acrostichum</em> (Pteridaceae), together with the mangrove palm <em>Nypa</em> and the climbing fern <em>Stenochlaena palustris</em> (Blechnaceae). The upper part of the studied section of the Kaliglagah Formation formed on the upper delta plain in an open freshwater swamp setting vegetated mainly with <em>Jussiaea</em> (Onagraceae)<em>, Pandanus</em> (Pandanaceae)<em>, Hanguana</em> (Hanguanaceae) and <em>Polygonum</em> (Polygonaceae). The <em>terra firma</em> vegetation during time of deposition of the succession consisted of grassy savanna in the lowlands, indicating a strongly seasonal climate, and montane forests with Podocarpaceae in the upper catchment. The swamp and <em>terra firma</em> vegetation succession are compared to that in Perning, East Java, and other Javanese hominid sites.</div><div>The Kalibiuk and lower part of the Kaliglagah Formation, and also the Pucangan Formation at the Perning <em>Homo erectus</em> site, yielded the age-restricted palynomorph <em>Stenochlaenidites papuanus</em>, the parent plant of which went extinct across Sunda during the early Pleistocene, emphasising the older age of these localities compared to other Javanese hominid sites, such as Sangiran and Trinil where this taxon is missing.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"339 ","pages":"Article 105352"},"PeriodicalIF":1.7,"publicationDate":"2025-04-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143864961","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Stellula meridionalis gen. et sp. nov., the oldest fossil flower from the Early Cretaceous of Argentina
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-04-09 DOI: 10.1016/j.revpalbo.2025.105350
Gabriela G. Puebla, Mercedes B. Prámparo
In this contribution, we describe a novel angiosperm floral axis, Stellula meridionalis gen. et sp. nov., consisting of a botryoid inflorescence, from the upper Aptian La Cantera Formation, San Luis Basin, central-western Argentina. Flowers are small, sessile and arranged distally on the inflorescences. Some specimens were found organically associated with leaves of “LC-Microphyll trifoliate”, a previously described and published fossil taxon. The leaves are nanophyllous, petiolate, with pinnately lobed or toothed margins, and the apex isn't preserved. Morphological features, such as pinnately lobed or toothed leaves with glandular margins, small trimerous actinomorphic flowers with floral organs in whorls, suggest an affinity with an early lineage of eudicots, likely within the Ranunculales. However, the absence of in situ pollen prevents definitive systematic assignment of the new taxon. Pollen analyses of dispersed taxa recovered from the same stratigraphic interval have revealed diverse angiosperm families, underscoring the complexity and increasing diversity of angiosperms in the mid-latitudes of South America during the Early Cretaceous.
{"title":"Stellula meridionalis gen. et sp. nov., the oldest fossil flower from the Early Cretaceous of Argentina","authors":"Gabriela G. Puebla,&nbsp;Mercedes B. Prámparo","doi":"10.1016/j.revpalbo.2025.105350","DOIUrl":"10.1016/j.revpalbo.2025.105350","url":null,"abstract":"<div><div>In this contribution, we describe a novel angiosperm floral axis, <em>Stellula meridionalis</em> gen. et sp. nov., consisting of a botryoid inflorescence, from the upper Aptian La Cantera Formation, San Luis Basin, central-western Argentina. Flowers are small, sessile and arranged distally on the inflorescences. Some specimens were found organically associated with leaves of “LC-Microphyll trifoliate”, a previously described and published fossil taxon. The leaves are nanophyllous, petiolate, with pinnately lobed or toothed margins, and the apex isn't preserved. Morphological features, such as pinnately lobed or toothed leaves with glandular margins, small trimerous actinomorphic flowers with floral organs in whorls, suggest an affinity with an early lineage of eudicots, likely within the Ranunculales. However, the absence of in situ pollen prevents definitive systematic assignment of the new taxon. Pollen analyses of dispersed taxa recovered from the same stratigraphic interval have revealed diverse angiosperm families, underscoring the complexity and increasing diversity of angiosperms in the mid-latitudes of South America during the Early Cretaceous.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"339 ","pages":"Article 105350"},"PeriodicalIF":1.7,"publicationDate":"2025-04-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143838353","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Rising Himalaya and climate change drive endemism in the Western Ghats: Fossil evidence insights
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-04-04 DOI: 10.1016/j.revpalbo.2025.105348
Harshita Bhatia , Gaurav Srivastava
Endemism, driven by geological and climatic transformations, is a hallmark of biodiversity hotspots. Fossil evidence offers unique insights into the historical biogeography and evolutionary trajectories of endemic taxa, particularly in biodiversity-rich regions like northeast India and the Western Ghats. This study reports the discovery of two Nothopegia species (Anacardiaceae) from late Oligocene sediments in the Makum Coalfield, Assam, northeast India. These fossils represent the earliest global record of the genus and display striking morphological similarities to the extant Nothopegia travancorica and N. castaneifolia, currently restricted to the Western Ghats, indicating a significant biogeographic shift over millions of years. Paleoclimatic and paleolatitudinal reconstructions suggest that the late Oligocene climate of northeast India mirrored the present-day equable climate of the Western Ghats, enabling the survival of Nothopegia in the region. However, the uplift of the Himalayan-Tibetan Plateau and a pronounced decline in the cold month mean temperature (CMMT) across northern and northeastern India likely drove the extinction of Nothopegia from these areas, confining it to the warmer environments of the Western Ghats. Present fossil evidence, along with previous fossil records of other plant taxa, underscores deep-time floristic connectivity between northeast India and the Western Ghats, likely facilitated by evergreen Paleogene forest corridors. These findings illuminate the biogeographic history of megadiverse ecosystems of South Asia and highlight the interplay between climatic shifts and geological events in shaping endemic biodiversity. Furthermore, the study demonstrates the critical role of paleobotanical data in guiding modern conservation strategies, particularly for relict taxa confined to isolated biodiversity hotspots.
{"title":"Rising Himalaya and climate change drive endemism in the Western Ghats: Fossil evidence insights","authors":"Harshita Bhatia ,&nbsp;Gaurav Srivastava","doi":"10.1016/j.revpalbo.2025.105348","DOIUrl":"10.1016/j.revpalbo.2025.105348","url":null,"abstract":"<div><div>Endemism, driven by geological and climatic transformations, is a hallmark of biodiversity hotspots. Fossil evidence offers unique insights into the historical biogeography and evolutionary trajectories of endemic taxa, particularly in biodiversity-rich regions like northeast India and the Western Ghats. This study reports the discovery of two <em>Nothopegia</em> species (Anacardiaceae) from late Oligocene sediments in the Makum Coalfield, Assam, northeast India. These fossils represent the earliest global record of the genus and display striking morphological similarities to the extant <em>Nothopegia travancorica</em> and <em>N. castaneifolia</em>, currently restricted to the Western Ghats, indicating a significant biogeographic shift over millions of years. Paleoclimatic and paleolatitudinal reconstructions suggest that the late Oligocene climate of northeast India mirrored the present-day equable climate of the Western Ghats, enabling the survival of <em>Nothopegia</em> in the region. However, the uplift of the Himalayan-Tibetan Plateau and a pronounced decline in the cold month mean temperature (CMMT) across northern and northeastern India likely drove the extinction of <em>Nothopegia</em> from these areas, confining it to the warmer environments of the Western Ghats. Present fossil evidence, along with previous fossil records of other plant taxa, underscores deep-time floristic connectivity between northeast India and the Western Ghats, likely facilitated by evergreen Paleogene forest corridors. These findings illuminate the biogeographic history of megadiverse ecosystems of South Asia and highlight the interplay between climatic shifts and geological events in shaping endemic biodiversity. Furthermore, the study demonstrates the critical role of paleobotanical data in guiding modern conservation strategies, particularly for relict taxa confined to isolated biodiversity hotspots.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"338 ","pages":"Article 105348"},"PeriodicalIF":1.7,"publicationDate":"2025-04-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143785918","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Corrigendum to FTIR spectra from grass pollen: A quest for species-level resolution of Poaceae and Cerealia-type pollen grains [Review of Palaeobotany and Palynology, 321 (2024): 105039]
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-03-29 DOI: 10.1016/j.revpalbo.2025.105333
F. Katsi , M.S. Kent , M. Jones , W.T. Fraser , P.E. Jardine , W. Eastwood , M. Mariani , C. Osborne , S. Edwards , B.H. Lomax
{"title":"Corrigendum to FTIR spectra from grass pollen: A quest for species-level resolution of Poaceae and Cerealia-type pollen grains [Review of Palaeobotany and Palynology, 321 (2024): 105039]","authors":"F. Katsi ,&nbsp;M.S. Kent ,&nbsp;M. Jones ,&nbsp;W.T. Fraser ,&nbsp;P.E. Jardine ,&nbsp;W. Eastwood ,&nbsp;M. Mariani ,&nbsp;C. Osborne ,&nbsp;S. Edwards ,&nbsp;B.H. Lomax","doi":"10.1016/j.revpalbo.2025.105333","DOIUrl":"10.1016/j.revpalbo.2025.105333","url":null,"abstract":"","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"338 ","pages":"Article 105333"},"PeriodicalIF":1.7,"publicationDate":"2025-03-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143843042","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Earliest thorny bamboo from Pleistocene of Asia characterizing spinescence and paleoclimatic adaptations in bamboos
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-03-28 DOI: 10.1016/j.revpalbo.2025.105347
Harshita Bhatia , Pushpa Kumari , N.H. Singh , Gaurav Srivastava
Spinescence—characterized by spines, prickles, and thorns—is a key defensive trait in plants, but is rare among bamboo genera. Its evolutionary history in bamboos remains poorly understood due to limited fossil evidence, with only a single previously documented specimen of a preserved node. Furthermore, the evolutionary ecology and paleoclimatic adaptations of bamboos during the Quaternary in Asia remain unclear due to a lack of fossil records. This study introduces Chimonobambusa manipurensis sp. nov., a well-preserved thorny bamboo fossil from the late Pleistocene of eastern India, marking the first Asian fossil record of thorny bamboo and the first Quaternary record from Asia. The fossil features nodes, internodes, nodal buds, and thorn scars, offering novel insights into bamboo spinescence and nodal morphology. C. manipurensis displays three well-preserved nodes, two complete internodes, prominently conserved nodal buds, and 3–4 thorn base scars along each nodal rim. Morphologically, it shares traits seen in modern Chimonobambusa Makino and is placed within the same genus. Together with a Pliocene–Pleistocene thorny bamboo record from Peru, this discovery suggests spinescence in bamboos likely emerged during the Neogene, with evolutionary adaptations continuing into the Pleistocene potentially as an adaptation to changing climatic conditions and increased herbivory pressures. Furthermore, it suggests that bamboos during Quaternary time in Asia were growing under warm and humid climatic conditions. This finding enhances our understanding of bamboo morphological evolution and paleoclimatic adaptations, filling a critical gap in the global fossil record.
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引用次数: 0
Palynology from the Foura Sandstone type section, Timor-Leste, and late Ladinian–Carnian (Middle–Upper Triassic) vegetation reconstruction from NW Australia
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-03-27 DOI: 10.1016/j.revpalbo.2025.105346
Daniel Peyrot , David W. Haig , Daniel Mantle , Peter Baillie , Arthur Mory , Myra Keep , Jacinto Soares , Joe Scibiorski , John Backhouse
A palynological analysis of the basinal volcaniclastic turbiditic Foura Sandstone Member within the Babulu Formation in Timor-Leste reveals rich assemblages including well-preserved material that correlates with the upper Ladinian–Carnian upper Staurosaccites quadrifidus–?lower Samaropollenites speciosus spore-pollen zones of Australia. The high diversity of conifer pollen in these assemblages indicates an association with microfloras from comparable latitudinal zones within Gondwana and an affiliation with the Onslow paleobiogeographic floral belt. The relationship between pollen and megafloral associations highlights the ecological flexibility of conifers, and their preeminent role in Triassic Gondwanan vegetation. The assemblages from the Foura Sandstone, including the new species Cadargasporites helbyi, Cadargasporites timorensis and Planctonites? comasii, point to the high diversity of vegetation in the area and the need for further studies.
{"title":"Palynology from the Foura Sandstone type section, Timor-Leste, and late Ladinian–Carnian (Middle–Upper Triassic) vegetation reconstruction from NW Australia","authors":"Daniel Peyrot ,&nbsp;David W. Haig ,&nbsp;Daniel Mantle ,&nbsp;Peter Baillie ,&nbsp;Arthur Mory ,&nbsp;Myra Keep ,&nbsp;Jacinto Soares ,&nbsp;Joe Scibiorski ,&nbsp;John Backhouse","doi":"10.1016/j.revpalbo.2025.105346","DOIUrl":"10.1016/j.revpalbo.2025.105346","url":null,"abstract":"<div><div>A palynological analysis of the basinal volcaniclastic turbiditic Foura Sandstone Member within the Babulu Formation in Timor-Leste reveals rich assemblages including well-preserved material that correlates with the upper Ladinian–Carnian upper <em>Staurosaccites quadrifidus</em>–?lower <em>Samaropollenites speciosus</em> spore-pollen zones of Australia. The high diversity of conifer pollen in these assemblages indicates an association with microfloras from comparable latitudinal zones within Gondwana and an affiliation with the Onslow paleobiogeographic floral belt. The relationship between pollen and megafloral associations highlights the ecological flexibility of conifers, and their preeminent role in Triassic Gondwanan vegetation. The assemblages from the Foura Sandstone, including the new species <em>Cadargasporites helbyi</em>, <em>Cadargasporites timorensis</em> and <em>Planctonites</em>? <em>comasii</em>, point to the high diversity of vegetation in the area and the need for further studies.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"338 ","pages":"Article 105346"},"PeriodicalIF":1.7,"publicationDate":"2025-03-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143776777","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Adding ‘flavour’ to past cuisines: First steps towards a phytolith reference collection of modern Mediterranean herbs
IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Pub Date : 2025-03-26 DOI: 10.1016/j.revpalbo.2025.105345
Carlos G. Santiago-Marrero , Cristina N. Patús , Costanza Dal Cin d'Agata , Teresa Garnatje , Juan José García-Granero
Most aromatic herbs belong to plants within the onion subfamily (Allioideae Herb.), the mint family (Lamiaceae Martinov), the parsley family (Apiaceae Lindl.) and the tarragon family (Asteraceae Bercht. & J.Presl), many of which are native to the Mediterranean. The culinary use of herbs has been textually documented in the eastern Mediterranean for over 3000 years. However, due to the nature of the archaeological record, where most macroscopic plant assemblages are preserved through charring, and the physiological characteristics of the plants themselves, herbs are largely underrepresented and have seldom been considered when assessing prehistoric culinary practices. Here, we present the results of a pilot modern phytolith reference collection of Mediterranean herbs to assess the potential of phytoliths in revealing ‘invisible’ plant ingredients in archaeological narratives. Phytoliths were observed in 48 of the 62 analysed reference samples. Although herbs are relatively poor phytolith producers, certain taxa produce distinctive morphotypes at different taxonomic levels that can potentially be used to identify the culinary uses of Mediterranean herbs in the archaeological record related to food preparation (e.g., residue analyses from food-processing artefacts, cooking vessels, charred food remains, etc.). In particular, anatomically connected silicified cells (silica skeletons) with potential taxonomic value were observed in species of the genus Mentha L. Moreover, species from the Apiaceae family, such as Daucus carota subsp. carota L. and Foeniculum vulgare Mill., produced massive multiseriate and pin-cushion trichomes with large multicellular stalks that could potentially hold taxonomic value.
{"title":"Adding ‘flavour’ to past cuisines: First steps towards a phytolith reference collection of modern Mediterranean herbs","authors":"Carlos G. Santiago-Marrero ,&nbsp;Cristina N. Patús ,&nbsp;Costanza Dal Cin d'Agata ,&nbsp;Teresa Garnatje ,&nbsp;Juan José García-Granero","doi":"10.1016/j.revpalbo.2025.105345","DOIUrl":"10.1016/j.revpalbo.2025.105345","url":null,"abstract":"<div><div>Most aromatic herbs belong to plants within the onion subfamily (A<span>llioideae</span> Herb.), the mint family (L<span>amiaceae</span> Martinov), the parsley family (A<span>piaceae</span> Lindl.) and the tarragon family (A<span>steraceae</span> Bercht. &amp; J.Presl), many of which are native to the Mediterranean. The culinary use of herbs has been textually documented in the eastern Mediterranean for over 3000 years. However, due to the nature of the archaeological record, where most macroscopic plant assemblages are preserved through charring, and the physiological characteristics of the plants themselves, herbs are largely underrepresented and have seldom been considered when assessing prehistoric culinary practices. Here, we present the results of a pilot modern phytolith reference collection of Mediterranean herbs to assess the potential of phytoliths in revealing ‘invisible’ plant ingredients in archaeological narratives. Phytoliths were observed in 48 of the 62 analysed reference samples. Although herbs are relatively poor phytolith producers, certain taxa produce distinctive morphotypes at different taxonomic levels that can potentially be used to identify the culinary uses of Mediterranean herbs in the archaeological record related to food preparation (e.g., residue analyses from food-processing artefacts, cooking vessels, charred food remains, etc.). In particular, anatomically connected silicified cells (silica skeletons) with potential taxonomic value were observed in species of the genus <em>Mentha</em> L. Moreover, species from the A<span>piaceae</span> family, such as <em>Daucus carota</em> subsp. <em>carota</em> L. and <em>Foeniculum vulgare</em> Mill., produced massive multiseriate and pin-cushion trichomes with large multicellular stalks that could potentially hold taxonomic value.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"338 ","pages":"Article 105345"},"PeriodicalIF":1.7,"publicationDate":"2025-03-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143739647","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
期刊
Review of Palaeobotany and Palynology
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