Pub Date : 2025-12-04DOI: 10.1016/j.revpalbo.2025.105482
Nina I. Gabarayeva , Valentina V. Grigorjeva
It was suggested that physicochemical processes, self-assembly and phase separation, are the hidden side of pollen wall formation. A new look at the developmental palynology as to “work-in-tandem” of well-known gene expression and underappreciated physical regularities allows a deeper understanding of exine development. The sequence of the developmental stages in Lupinus exine has been analyzed based on the above idea. To check the above idea, a modeling of exine-like pattern was carried out in vitro with colloidal mixtures of surfactants, analogous to those in natural anther. Flower buds of different size were collected from the Garden of the Komarov Botanical Institute, St. Petersburg, for several seasons. After fixation of the Lupinus material, sections were prepared and examined with TEM and SEM. For modeling exine development in vitro, our own method was used to obtain simulations. The successive developmental structures observed within the microspore periplasmic space have occurred to be the same as in the typical micellar self-assembly sequence in colloidal system of surfactants. Simultaneously, signs of phase separation in the fluid of the periplasmic space were evident. As was expected, several exine-like simulations of the Lupinus exine structures were obtained in our experiments. Pure physicochemical processes are capable to build exine-like patterns. Hence, physical processes share influence on exine development with genome. This confirms a value of interdisciplinary approach in the field of developmental biology.
{"title":"Pollen wall development in Lupinus polyphyllus: Looking for underlying mechanisms, with in vitro simulation of exine","authors":"Nina I. Gabarayeva , Valentina V. Grigorjeva","doi":"10.1016/j.revpalbo.2025.105482","DOIUrl":"10.1016/j.revpalbo.2025.105482","url":null,"abstract":"<div><div>It was suggested that physicochemical processes, self-assembly and phase separation, are the hidden side of pollen wall formation. A new look at the developmental palynology as to “work-in-tandem” of well-known gene expression and underappreciated physical regularities allows a deeper understanding of exine development. The sequence of the developmental stages in <em>Lupinus</em> exine has been analyzed based on the above idea. To check the above idea, a modeling of exine-like pattern was carried out <em>in vitro</em> with colloidal mixtures of surfactants, analogous to those in natural anther. Flower buds of different size were collected from the Garden of the Komarov Botanical Institute, St. Petersburg, for several seasons. After fixation of the <em>Lupinus</em> material, sections were prepared and examined with TEM and SEM. For modeling exine development <em>in vitro</em>, our own method was used to obtain simulations. The successive developmental structures observed within the microspore periplasmic space have occurred to be the same as in the typical micellar self-assembly sequence in colloidal system of surfactants. Simultaneously, signs of phase separation in the fluid of the periplasmic space were evident. As was expected, several exine-like simulations of the <em>Lupinus</em> exine structures were obtained in our experiments. Pure physicochemical processes are capable to build exine-like patterns. Hence, physical processes share influence on exine development with genome. This confirms a value of interdisciplinary approach in the field of developmental biology.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"346 ","pages":"Article 105482"},"PeriodicalIF":1.7,"publicationDate":"2025-12-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145694769","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}
Pub Date : 2025-12-04DOI: 10.1016/j.revpalbo.2025.105479
J.B. Innes , J.J. Blackford , V. Standen , C. Orton
The paper assesses contemporary pollen and non-pollen palynomorph (NPP) distribution along a woodland to heathland transect, and tests the ecological preferences of the recorded NPP taxa, providing modern analogue information to assist in the interpretation of palaeoecological data. Pollen, microcharcoal, fungal spores and other NPPs are analysed from surface sediment samples collected from Quercus-dominated woodland and mixed heathland (Calluna, Vaccinium, Poaceae, Juncus, Pteridium) from an upland area in North East England and the microfossil assemblage data are compared with the actual vegetation cover at the sampling points. The microfossil data clearly indicate the position of the woodland-heathland boundary to within 2–10 m. The transitional zone is shown to be narrow, but of distinctive palynological character. The ecological meaning of several NPPs is either confirmed or suggested. NPP and pollen assemblages vary considerable over distances of only 2–5 m across the transitional samples, whereas very similar microfossil assemblages occur within the two main woodland and heathland vegetation units, even where plant species change in relative abundance. Woodland, heathland and transitional assemblages are clearly differentiated. NPP deposition occurs close to their source, and many types have well defined ecological affinities and are sensitive environmental indicators, while others are more cosmopolitan.
{"title":"Modern pollen and NPP assemblages across an abrupt woodland/heathland transition in upland north east England: Implications for taphonomy and palaeoecological interpretation","authors":"J.B. Innes , J.J. Blackford , V. Standen , C. Orton","doi":"10.1016/j.revpalbo.2025.105479","DOIUrl":"10.1016/j.revpalbo.2025.105479","url":null,"abstract":"<div><div>The paper assesses contemporary pollen and non-pollen palynomorph (NPP) distribution along a woodland to heathland transect, and tests the ecological preferences of the recorded NPP taxa, providing modern analogue information to assist in the interpretation of palaeoecological data. Pollen, microcharcoal, fungal spores and other NPPs are analysed from surface sediment samples collected from <em>Quercus</em>-dominated woodland and mixed heathland (<em>Calluna, Vaccinium,</em> Poaceae<em>, Juncus, Pteridium</em>) from an upland area in North East England and the microfossil assemblage data are compared with the actual vegetation cover at the sampling points. The microfossil data clearly indicate the position of the woodland-heathland boundary to within 2–10 m. The transitional zone is shown to be narrow, but of distinctive palynological character. The ecological meaning of several NPPs is either confirmed or suggested. NPP and pollen assemblages vary considerable over distances of only 2–5 m across the transitional samples, whereas very similar microfossil assemblages occur within the two main woodland and heathland vegetation units, even where plant species change in relative abundance. Woodland, heathland and transitional assemblages are clearly differentiated. NPP deposition occurs close to their source, and many types have well defined ecological affinities and are sensitive environmental indicators, while others are more cosmopolitan.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"346 ","pages":"Article 105479"},"PeriodicalIF":1.7,"publicationDate":"2025-12-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145749736","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}
Pub Date : 2025-12-02DOI: 10.1016/j.revpalbo.2025.105483
Marine Rousseau , Philippe Sorrel , Benjamin Diètre , Morana Čaušević-Bully , Hervé Richard
We present the first high-resolution palynological and multiproxy reconstruction from a coastal doline in the Kvarner Archipelago (northeastern Adriatic). A continuous sediment core from Osor Lake documents more than three millennia of vegetation change, human impact, and hydrological shifts since the Bronze Age. The record reveals three major phases of landscape transformation: (i) dense deciduous forests (3400–2550 cal BP) with initial signs of clearance; (ii) a progressive landscape opening from 2550 cal BP, marked by expanding grasslands and cultivated fields; and (iii) intensified deforestation and arboriculture after ∼ 800 cal BP. The introduction of Juglans and Castanea sativa between 2200 and 1200 cal BP, together with increasing Olea europaea, reflects evolving Mediterranean agricultural strategies. Charcoal peaks coincide with forest decline, indicating recurrent fire use for land management. This study establishes Osor Lake as a benchmark record for late Holocene land-use history in the northeastern Adriatic and demonstrates how human activities progressively reshaped Mediterranean karst landscapes.
我们提出了第一个高分辨率的孢粉和多代理重建,从Kvarner群岛(亚得里亚海东北部)的海岸线。奥索尔湖的连续沉积物岩心记录了自青铜时代以来3000多年的植被变化、人类影响和水文变化。该记录揭示了景观转变的三个主要阶段:(i)茂密的落叶林(3400-2550 cal BP)有最初的砍伐迹象;(ii)从2550 cal BP开始,以扩大草地和耕地为标志的递进景观;(iii)约800 cal BP之后森林砍伐和树木栽培加剧。在2200至1200 cal BP之间,核桃和番栗的引入,以及欧洲油橄榄的增加,反映了地中海农业战略的演变。木炭峰值与森林衰退相吻合,表明土地管理经常使用火。本研究确立了Osor湖作为亚得里亚海东北部晚全新世土地利用历史的基准记录,并展示了人类活动如何逐步重塑地中海喀斯特景观。
{"title":"Vegetation changes and human activities since the Bronze Age (late Holocene) in a coastal doline of the Kvarner archipelago (Croatia)","authors":"Marine Rousseau , Philippe Sorrel , Benjamin Diètre , Morana Čaušević-Bully , Hervé Richard","doi":"10.1016/j.revpalbo.2025.105483","DOIUrl":"10.1016/j.revpalbo.2025.105483","url":null,"abstract":"<div><div>We present the first high-resolution palynological and multiproxy reconstruction from a coastal doline in the Kvarner Archipelago (northeastern Adriatic). A continuous sediment core from Osor Lake documents more than three millennia of vegetation change, human impact, and hydrological shifts since the Bronze Age. The record reveals three major phases of landscape transformation: (i) dense deciduous forests (3400–2550 cal BP) with initial signs of clearance; (ii) a progressive landscape opening from 2550 cal BP, marked by expanding grasslands and cultivated fields; and (iii) intensified deforestation and arboriculture after ∼<!--> <!-->800 cal BP. The introduction of <em>Juglans</em> and <em>Castanea sativa</em> between 2200 and 1200 cal BP, together with increasing <em>Olea europaea</em>, reflects evolving Mediterranean agricultural strategies. Charcoal peaks coincide with forest decline, indicating recurrent fire use for land management. This study establishes Osor Lake as a benchmark record for late Holocene land-use history in the northeastern Adriatic and demonstrates how human activities progressively reshaped Mediterranean karst landscapes.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"345 ","pages":"Article 105483"},"PeriodicalIF":1.7,"publicationDate":"2025-12-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145737101","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}
Palynological analyses are performed on the imprecisely dated ‘Upper Cretaceous–lower Eocene’ marly and marly limestones succession from the Thare section at Arbaa Ayacha, western External Rif (northwestern Morocco) to reassess the previous calcareous microplankton-based age determination of the sediments. The succession yields well to moderately preserved palynological associations that are mainly composed of organic-walled dinoflagellate cysts, suitable for biostratigraphic analysis. The sediments are here reassessed as being of middle Bartonian age using the recently well-calibrated distribution patterns of several index taxa like Glaphyrocysta semitecta, and Rhombodinium perforatum. These, taken together with the composition of the background assemblages allow quite precise designation of the section to the interval corresponding to magnetochrons C18n.1r to C18n.1n following correlation to the Bartonian/Priabonian Global Stratotype Section and Point (GSSP) section at Alano di Piave, NE Italy. Our results further underline the potential of marine palynological analysis emphasizing organic-walled dinoflagellate cysts in biostratigraphic and paleoenvironmental analyses of the Mediterranean Paleogene.
孢粉学分析对来自Arbaa Ayacha西部外裂谷(摩洛哥西北部)Thare剖面的“上白垩世-下始新世”泥灰岩和泥灰岩演替进行了不精确的年代分析,以重新评估之前基于钙质微浮游生物的沉积物年龄测定。该演替产生了保存良好至中等程度的孢粉组合,主要由有机壁鞭毛藻包囊组成,适合生物地层分析。在这里,沉积物被重新评估为中巴尔顿时代,使用了最近校准好的几个指数分类群,如半葡萄球菌和穿孔菱形虫的分布模式。结合背景组合的组成,可以相当精确地指定该剖面对应于磁时线C18n的间隔。1r到C18n。与意大利东北部Alano di Piave的Bartonian/Priabonian全球层型剖面和点(GSSP)剖面相关。我们的研究结果进一步强调了以有机壁鞭毛藻囊为重点的海洋孢粉学分析在地中海古近系生物地层和古环境分析中的潜力。
{"title":"Middle Eocene dinoflagellate cyst biostratigraphy from the southwestern Tethyan margin: Revised age assessments of sediments near Larache Province, northwestern Morocco","authors":"Salma Aboutofail , Hamid Slimani , Henk Brinkhuis , Ali Soliman , Daniel Ţabără , Imad Tmimne , Hassan Jbari , Amine Talih , Imane Mahboub","doi":"10.1016/j.revpalbo.2025.105481","DOIUrl":"10.1016/j.revpalbo.2025.105481","url":null,"abstract":"<div><div>Palynological analyses are performed on the imprecisely dated ‘Upper Cretaceous–lower Eocene’ marly and marly limestones succession from the Thare section at Arbaa Ayacha, western External Rif (northwestern Morocco) to reassess the previous calcareous microplankton-based age determination of the sediments. The succession yields well to moderately preserved palynological associations that are mainly composed of organic-walled dinoflagellate cysts, suitable for biostratigraphic analysis. The sediments are here reassessed as being of middle Bartonian age using the recently well-calibrated distribution patterns of several index taxa like <em>Glaphyrocysta semitecta,</em> and <em>Rhombodinium perforatum.</em> These, taken together with the composition of the background assemblages allow quite precise designation of the section to the interval corresponding to magnetochrons C18n.1r to C18n.1n following correlation to the Bartonian/Priabonian Global Stratotype Section and Point (GSSP) section at Alano di Piave, NE Italy. Our results further underline the potential of marine palynological analysis emphasizing organic-walled dinoflagellate cysts in biostratigraphic and paleoenvironmental analyses of the Mediterranean Paleogene.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"346 ","pages":"Article 105481"},"PeriodicalIF":1.7,"publicationDate":"2025-11-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145694771","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}
Pub Date : 2025-11-27DOI: 10.1016/j.revpalbo.2025.105480
Xiaoyi Shen , Yanbin Hao , Yanfen Wang , Xiyue Luo , Junxing Du , Aizhi Sun , Jianqing Du
Accurately reconstructing Holocene vegetation dynamics in ecologically sensitive regions is critical for understanding past climate–vegetation interactions and predicting future ecosystem responses. The Yanshan region, a key climatic and ecological transition zone in northern China, has experienced significant vegetation changes during the Holocene, yet previous reconstructions have largely relied on qualitative or semi-quantitative approaches, with limited spatial coverage and temporal reconstruction. In this study, we applied biomization of 33 high-quality fossil pollen records to quantitatively reconstruct the spatiotemporal vegetation succession of the Yanshan region over the past 12,000 years. Our results showed a general trend of steppe–forest–steppe transitions, primarily driven by variations in East Asian summer monsoon (EASM) precipitation. Spatially, vegetation characteristics and succession differ significantly across topographic units. A significant increase in forest cover occurred in the plain after ∼ 5 ka BP, which contrasted with the similar Holocene pattern in the plateau and mountain. This difference may be attributed to transgression of the Bohai Sea into the plain before ∼ 6 ka BP. Notably, a reversal of forest decline occurred after 3 ka BP, particularly in the plain and mountain areas, which is attributed to intensified human activities, including economic tree cultivation and secondary forest expansion. These findings highlight the dominant role of precipitation in regulating regional vegetation, while underscoring the increasing influence of anthropogenic factors in the late Holocene landscape transformation. This study provides a robust quantitative framework for understanding long-term vegetation dynamics and offers critical insights for ecological restoration and climate adaptation strategies in northern China.
准确重建生态敏感区全新世植被动态对于理解过去气候-植被相互作用和预测未来生态系统响应至关重要。燕山地区是中国北方重要的气候生态过渡带,在全新世期间经历了显著的植被变化,但以往的重建主要依赖于定性或半定量方法,空间覆盖和时间重建有限。通过对33份高质量花粉化石记录的生物化处理,对燕山地区近12000年来的植被演替进行了定量重建。研究结果表明,东亚夏季风(EASM)降水变化主要驱动了草原-森林-草原过渡的总体趋势。在空间上,不同地形单元的植被特征和演替存在显著差异。在~ 5 ka BP之后,平原的森林覆盖出现了显著的增加,这与高原和山地的类似全新世格局形成了对比。这种差异可能与渤海在~ 6ka BP之前的海侵有关。值得注意的是,在3 ka BP之后,森林衰退发生逆转,特别是在平原和山区,这归因于人类活动的加剧,包括经济树木的种植和次生林的扩张。这些发现强调了降水在区域植被调节中的主导作用,同时也强调了人类活动对晚全新世景观转变的影响越来越大。该研究为了解中国北方植被的长期动态提供了一个强有力的定量框架,并为中国北方生态恢复和气候适应策略提供了重要见解。
{"title":"Quantitative reconstruction of Holocene vegetation dynamics and their drivers in the Yanshan region, northern China","authors":"Xiaoyi Shen , Yanbin Hao , Yanfen Wang , Xiyue Luo , Junxing Du , Aizhi Sun , Jianqing Du","doi":"10.1016/j.revpalbo.2025.105480","DOIUrl":"10.1016/j.revpalbo.2025.105480","url":null,"abstract":"<div><div>Accurately reconstructing Holocene vegetation dynamics in ecologically sensitive regions is critical for understanding past climate–vegetation interactions and predicting future ecosystem responses. The Yanshan region, a key climatic and ecological transition zone in northern China, has experienced significant vegetation changes during the Holocene, yet previous reconstructions have largely relied on qualitative or semi-quantitative approaches, with limited spatial coverage and temporal reconstruction. In this study, we applied biomization of 33 high-quality fossil pollen records to quantitatively reconstruct the spatiotemporal vegetation succession of the Yanshan region over the past 12,000 years. Our results showed a general trend of steppe–forest–steppe transitions, primarily driven by variations in East Asian summer monsoon (EASM) precipitation. Spatially, vegetation characteristics and succession differ significantly across topographic units. A significant increase in forest cover occurred in the plain after ∼<!--> <!-->5 ka BP, which contrasted with the similar Holocene pattern in the plateau and mountain. This difference may be attributed to transgression of the Bohai Sea into the plain before ∼<!--> <!-->6 ka BP. Notably, a reversal of forest decline occurred after 3 ka BP, particularly in the plain and mountain areas, which is attributed to intensified human activities, including economic tree cultivation and secondary forest expansion. These findings highlight the dominant role of precipitation in regulating regional vegetation, while underscoring the increasing influence of anthropogenic factors in the late Holocene landscape transformation. This study provides a robust quantitative framework for understanding long-term vegetation dynamics and offers critical insights for ecological restoration and climate adaptation strategies in northern China.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"346 ","pages":"Article 105480"},"PeriodicalIF":1.7,"publicationDate":"2025-11-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145625411","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}
Pub Date : 2025-11-26DOI: 10.1016/j.revpalbo.2025.105477
Zoya M. Tsymbalyuk , Daniella Ivanova , Lyudmila M. Nitsenko
Based on morphological, morphometric and molecular data, Axyris, Ceratocarpus and Krascheninnikovia, were classified to the subtribe Axyridinae, and later this group was elevated to tribe Axyrideae (Chenopodiaceae / Amaranthaceae). Previously, the representatives of these three genera, together with Grayia, have been included in the subtribe Eurotiinae. Their relationships are poorly understood; the position of Grayia still remains unclear. Considering that palynomorphological traits can be useful for angiosperm taxonomy, the aim of this research was to provide detailed data on the Axyrideae and Grayia pollen characters and to evaluate their taxonomic significance. Pollen morphology of 13 specimens belonging to seven species of the genera Axyris, Ceratocarpus, Grayia (including Zuckia), and Krascheninnikovia was studied using light and scanning electron microscopy. Pollen grains are pantoporate, spheroidal, mainly circular in outline, small or medium-sized. Exine sculpture and pore membranes are nanoechinate, tectum is psilate-perforate. The data obtained showed that species and genera can be identified based on palynomorphological features, especially the pollen diameter, pore number, pore diameter, distance between pores and between pore centres, nanoechini density, number of nanoechini on pore membranes, exine thickness, and structure of columellae. Exine structure (columellae) of pollen grains of all species was analysed for the first time in the present study. UPGMA dendrogram, based on quantitative pollen traits (nanoechini height, width at the base, number per 4 μm2, and number on pore membrane), supported the differentiation of genera. The data obtained confirm the close relationships between tribe Axyrideae (Axyris, Ceratocarpus, Krascheninnikovia) and Grayia (including Zuckia). This study highlights the importance of palynomorphological characters for the taxonomy.
{"title":"Comparative pollen morphology of the genera Axyris L., Ceratocarpus L., Grayia Hook. & Arn. and Krascheninnikovia Gueldenst. (Amaranthaceae)","authors":"Zoya M. Tsymbalyuk , Daniella Ivanova , Lyudmila M. Nitsenko","doi":"10.1016/j.revpalbo.2025.105477","DOIUrl":"10.1016/j.revpalbo.2025.105477","url":null,"abstract":"<div><div>Based on morphological, morphometric and molecular data, <em>Axyris</em>, <em>Ceratocarpus</em> and <em>Krascheninnikovia,</em> were classified to the subtribe Axyridinae, and later this group was elevated to tribe Axyrideae (Chenopodiaceae / Amaranthaceae). Previously, the representatives of these three genera, together with <em>Grayia</em>, have been included in the subtribe Eurotiinae. Their relationships are poorly understood; the position of <em>Grayia</em> still remains unclear. Considering that palynomorphological traits can be useful for angiosperm taxonomy, the aim of this research was to provide detailed data on the Axyrideae and <em>Grayia</em> pollen characters and to evaluate their taxonomic significance. Pollen morphology of 13 specimens belonging to seven species of the genera <em>Axyris</em>, <em>Ceratocarpus</em>, <em>Grayia</em> (including <em>Zuckia</em>), and <em>Krascheninnikovia</em> was studied using light and scanning electron microscopy<em>.</em> Pollen grains are pantoporate, spheroidal, mainly circular in outline, small or medium-sized. Exine sculpture and pore membranes are nanoechinate, tectum is psilate-perforate. The data obtained showed that species and genera can be identified based on palynomorphological features, especially the pollen diameter, pore number, pore diameter, distance between pores and between pore centres, nanoechini density, number of nanoechini on pore membranes, exine thickness, and structure of columellae. Exine structure (columellae) of pollen grains of all species was analysed for the first time in the present study. UPGMA dendrogram, based on quantitative pollen traits (nanoechini height, width at the base, number per 4 μm<sup>2</sup>, and number on pore membrane), supported the differentiation of genera. The data obtained confirm the close relationships between tribe Axyrideae (<em>Axyris</em>, <em>Ceratocarpus</em>, <em>Krascheninnikovia</em>) and <em>Grayia</em> (including <em>Zuckia</em>). This study highlights the importance of palynomorphological characters for the taxonomy.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"345 ","pages":"Article 105477"},"PeriodicalIF":1.7,"publicationDate":"2025-11-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145685340","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}
Pub Date : 2025-11-23DOI: 10.1016/j.revpalbo.2025.105475
P.E. Santamarina , V.D. Barreda , M.S. González Estebenet , V. Guler , E.S. Bellosi , F. Novas
We present the palynological assemblages recovered from the upper part of the La Anita and Cerro Fortaleza formations (Campanian) from SW Patagonia, Argentina. A total of 73 continental species and 11 dinoflagellate cysts species were identified in this study. Continental species comprise 17 bryophytes and lycophytes, 20 ferns, 14 gymnosperms, 21 angiosperms, and 1 of uncertain affinity. The palynofloras are strongly dominated by gymnosperms, with angiosperms and ferns as secondary components. Cluster analysis employed to explore floristic similarities with Campanian–Maastrichtian palynofloras reveals two main groups: one grouping the palynofloras presented here and another grouping Campanian–Maastrichtian palynofloras from southern South America and the Antarctic Peninsula. The occurrence of spores attributable to Salviniales and Anemiaceae, along with pollen grains referable to Symplocaceae, Aquifoliaceae, and Arecaceae suggests a humid and temperate climate. The presence of Odontochitina porifera and Nelsoniella aceras suggests a late Santonian–early Maastrichtian age of deposition. In addition, continental palynological assemblages are consistent with the Campanian age established by radiometric dating. A comparative assessment of angiosperm diversity and abundance within these assemblages and published records indicates that angiosperms had not yet become the dominant floral component in southern Patagonia during the Late Cretaceous, in contrast to coeval floras at similar paleolatitudes in the Northern Hemisphere. However, further high-resolution palynological analyses are needed to refine our understanding of floristic composition, biogeographic patterns, and the time and mode of angiosperm diversification in southern Patagonia during the late Cretaceous.
{"title":"Palynological analysis of the La Anita and Cerro Fortaleza formations (Campanian), southern margin of the Viedma Lake, Santa Cruz Province, Argentina","authors":"P.E. Santamarina , V.D. Barreda , M.S. González Estebenet , V. Guler , E.S. Bellosi , F. Novas","doi":"10.1016/j.revpalbo.2025.105475","DOIUrl":"10.1016/j.revpalbo.2025.105475","url":null,"abstract":"<div><div>We present the palynological assemblages recovered from the upper part of the La Anita and Cerro Fortaleza formations (Campanian) from SW Patagonia, Argentina. A total of 73 continental species and 11 dinoflagellate cysts species were identified in this study. Continental species comprise 17 bryophytes and lycophytes, 20 ferns, 14 gymnosperms, 21 angiosperms, and 1 of uncertain affinity. The palynofloras are strongly dominated by gymnosperms, with angiosperms and ferns as secondary components. Cluster analysis employed to explore floristic similarities with Campanian–Maastrichtian palynofloras reveals two main groups: one grouping the palynofloras presented here and another grouping Campanian–Maastrichtian palynofloras from southern South America and the Antarctic Peninsula. The occurrence of spores attributable to Salviniales and Anemiaceae, along with pollen grains referable to Symplocaceae, Aquifoliaceae, and Arecaceae suggests a humid and temperate climate. The presence of <em>Odontochitina porifera</em> and <em>Nelsoniella aceras</em> suggests a late Santonian–early Maastrichtian age of deposition. In addition, continental palynological assemblages are consistent with the Campanian age established by radiometric dating. A comparative assessment of angiosperm diversity and abundance within these assemblages and published records indicates that angiosperms had not yet become the dominant floral component in southern Patagonia during the Late Cretaceous, in contrast to coeval floras at similar paleolatitudes in the Northern Hemisphere. However, further high-resolution palynological analyses are needed to refine our understanding of floristic composition, biogeographic patterns, and the time and mode of angiosperm diversification in southern Patagonia during the late Cretaceous.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"345 ","pages":"Article 105475"},"PeriodicalIF":1.7,"publicationDate":"2025-11-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145618568","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}
Pub Date : 2025-11-19DOI: 10.1016/j.revpalbo.2025.105476
Osvaldo A. Conde , Roberto R. Pujana , Gustavo A. Correa , M. Lucía Balarino
This contribution describes a new gymnospermous fossil stem from western Gondwana. Barrealoxylon nelsonii nov. gen. et sp. was recovered from the Pituil Formation (Early Pennsylvanian), Calingasta-Uspallata Basin in San Juan Province, Argentina. The new species is characterized by a septate pith and mesarch primary xylem. The secondary xylem shows distinct growth ring boundaries, tracheids with uniseriate to triseriate araucarian pits in radial walls, pits in tangential walls, and cross-fields with 1–2, rarely 3, “window-like” (= fenestriform) pits. The combination of a septate pith and the primary and secondary xylem characteristics supports its assignment to the Cordaitales, providing further evidence for the presence of this group in southwestern Gondwana. The secondary xylem of the new stem has D-type growth rings, indicative of uniform growth conditions followed by a final stage of reduced vascular cambium activity. This type of growth ring is consistent with the high-humidity climatic conditions that prevailed during the Terminal Glacial Stage in western Gondwana.
{"title":"Barrealoxylon nelsonii gen. et sp. nov., a new Pennsylvanian (Carboniferous) fossil stem from Gondwana: Botanical affinity and paleoclimatic implications","authors":"Osvaldo A. Conde , Roberto R. Pujana , Gustavo A. Correa , M. Lucía Balarino","doi":"10.1016/j.revpalbo.2025.105476","DOIUrl":"10.1016/j.revpalbo.2025.105476","url":null,"abstract":"<div><div>This contribution describes a new gymnospermous fossil stem from western Gondwana. <em>Barrealoxylon nelsonii</em> nov. gen. et sp. was recovered from the Pituil Formation (Early Pennsylvanian), Calingasta-Uspallata Basin in San Juan Province, Argentina. The new species is characterized by a septate pith and mesarch primary xylem. The secondary xylem shows distinct growth ring boundaries, tracheids with uniseriate to triseriate araucarian pits in radial walls, pits in tangential walls, and cross-fields with 1–2, rarely 3, “window-like” (=<!--> <!-->fenestriform) pits. The combination of a septate pith and the primary and secondary xylem characteristics supports its assignment to the Cordaitales, providing further evidence for the presence of this group in southwestern Gondwana. The secondary xylem of the new stem has D-type growth rings, indicative of uniform growth conditions followed by a final stage of reduced vascular cambium activity. This type of growth ring is consistent with the high-humidity climatic conditions that prevailed during the Terminal Glacial Stage in western Gondwana.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"345 ","pages":"Article 105476"},"PeriodicalIF":1.7,"publicationDate":"2025-11-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145571944","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}
Pub Date : 2025-11-08DOI: 10.1016/j.revpalbo.2025.105467
Lan-Xing Wei, Cun-Lin Xin, Zhi -Peng Jiao, Fang-Fang Zhang, Hong Li
Coniopteris (Dicksoniaceae) is a species-rich and diverse Mesozoic fern genus. Based on well-preserved material from the Middle Jurassic Yaojie Formation in the Baojishan Basin, Gansu, China, we combine macromorphology with microstructural characters to describe a new species—Coniopteris baojishanensis Wei et Xin, sp. nov. The frond is lanceolate and at least bipinnate; the ultimate pinnae bear a basal pair of heteromorphic pinnules; the rachis bears a conspicuous longitudinal ridge. Sterile pinnules are elongate-ovate; fertile pinnules are slightly contracted, ovate. A preliminary analysis of the evolutionary distribution of heteromorphic pinnules in Coniopteris indicates first appearance in the Early Jurassic, a peak in the Middle Jurassic, and marked decline by the Cretaceous. We interpret heteromorphic pinnules as an adaptation to moist, low-light understory conditions: by enlarging area or increasing the degree of dissection, they increase light capture and enhance photosynthetic efficiency, thereby improving competitive ability within the community. This study enriches the Chinese fossil record of Coniopteris and provides new clues to the formation of its heteromorphic pinnules.
刺蕨属(刺蕨科)是中生代蕨类植物中种类丰富、种类多样的一个属。根据甘肃宝鸡山盆地中侏罗统姚界组保存完好的材料,结合宏观形态和微观结构特征,描述了一个新种——coniopteris baojishanensis Wei et Xin, sp. 11。末级羽片生一对异型小羽片;轴有明显的纵脊。不育小穗状花序拉长卵形;可育小叶稍收缩,卵形。对锥翼兽异型小尖的演化分布进行初步分析,表明锥翼兽的异型小尖最早出现于早侏罗世,在中侏罗世达到顶峰,在白垩纪显著下降。我们将异型小叶解释为对潮湿、低光照林下条件的适应:它们通过扩大面积或增加解剖程度,增加光捕获和提高光合效率,从而提高群落内的竞争能力。本研究丰富了刺蕨属的中国化石记录,为其异型小尖的形成提供了新的线索。
{"title":"A new Coniopteris (Dicksoniaceae) from the Middle Jurassic of the Baojishan Basin, Gansu, China, with discussion on its heteromorphic pinnule characteristics","authors":"Lan-Xing Wei, Cun-Lin Xin, Zhi -Peng Jiao, Fang-Fang Zhang, Hong Li","doi":"10.1016/j.revpalbo.2025.105467","DOIUrl":"10.1016/j.revpalbo.2025.105467","url":null,"abstract":"<div><div><em>Coniopteris</em> (Dicksoniaceae) is a species-rich and diverse Mesozoic fern genus. Based on well-preserved material from the Middle Jurassic Yaojie Formation in the Baojishan Basin, Gansu, China, we combine macromorphology with microstructural characters to describe a new species—<em>Coniopteris baojishanensis</em> Wei et Xin, sp. nov. The frond is lanceolate and at least bipinnate; the ultimate pinnae bear a basal pair of heteromorphic pinnules; the rachis bears a conspicuous longitudinal ridge. Sterile pinnules are elongate-ovate; fertile pinnules are slightly contracted, ovate. A preliminary analysis of the evolutionary distribution of heteromorphic pinnules in <em>Coniopteris</em> indicates first appearance in the Early Jurassic, a peak in the Middle Jurassic, and marked decline by the Cretaceous. We interpret heteromorphic pinnules as an adaptation to moist, low-light understory conditions: by enlarging area or increasing the degree of dissection, they increase light capture and enhance photosynthetic efficiency, thereby improving competitive ability within the community. This study enriches the Chinese fossil record of <em>Coniopteris</em> and provides new clues to the formation of its heteromorphic pinnules.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"344 ","pages":"Article 105467"},"PeriodicalIF":1.7,"publicationDate":"2025-11-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145519742","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}
Pub Date : 2025-11-04DOI: 10.1016/j.revpalbo.2025.105466
Mohammad Firoze Quamar , Nagendra Prasad , Biswajeet Thakur , Maneesha Muraleedharan ET
Herbivory plays a crucial role as a long-term driver of ecosystem changes. Understanding the interactions between herbivores and ecosystems is particularly important for shaping conservation policies, especially those focused on re-wilding. Additionally, understanding changes in the abundance of large herbivores over time and assessing the role of key animal species in disturbance regimes, biodiversity dynamics, and ecosystem resilience remains a significant challenge in long-term ecological studies. Spores specific to herbivore dung offer a valuable source of information on past herbivore populations. Sporormiella, a coprophilous fungal spore that grows on herbivore dung, serves as an important proxy for reconstructing the presence and/or abundance of megaherbivores, livestock density, grazing activity (pastoralism), human impact, extinction events, and the effects of husbandry practices on the natural environment over time and across regions. In India, the application of Sporormiella as a proxy for herbivore presence and abundance remains at an early stage and requires further systematic testing. This review article aims to evaluate the potential of Sporormiella in reconstructing herbivore presence and abundance across different temporal and spatial scales in India. The synthesis of Sporormiella records from both modern and the Holocene sediment samples provides insights into past herbivore densities. Additionally, this study discusses various factors influencing the composition of the spores of coprophilous fungi, and the abundance of Sporormiella, potential constraints on their preservation in certain settings, and the limitations of current research. This research review article also outlines broader implications and directions for the future research.
{"title":"Assessment of herbivore densities using Sporormiella as a palynological proxy: Indian context and the way forward","authors":"Mohammad Firoze Quamar , Nagendra Prasad , Biswajeet Thakur , Maneesha Muraleedharan ET","doi":"10.1016/j.revpalbo.2025.105466","DOIUrl":"10.1016/j.revpalbo.2025.105466","url":null,"abstract":"<div><div>Herbivory plays a crucial role as a long-term driver of ecosystem changes. Understanding the interactions between herbivores and ecosystems is particularly important for shaping conservation policies, especially those focused on re-wilding. Additionally, understanding changes in the abundance of large herbivores over time and assessing the role of key animal species in disturbance regimes, biodiversity dynamics, and ecosystem resilience remains a significant challenge in long-term ecological studies. Spores specific to herbivore dung offer a valuable source of information on past herbivore populations. <em>Sporormiella</em>, a coprophilous fungal spore that grows on herbivore dung, serves as an important proxy for reconstructing the presence and/or abundance of megaherbivores, livestock density, grazing activity (pastoralism), human impact, extinction events, and the effects of husbandry practices on the natural environment over time and across regions. In India, the application of <em>Sporormiella</em> as a proxy for herbivore presence and abundance remains at an early stage and requires further systematic testing. This review article aims to evaluate the potential of <em>Sporormiella</em> in reconstructing herbivore presence and abundance across different temporal and spatial scales in India. The synthesis of <em>Sporormiella</em> records from both modern and the Holocene sediment samples provides insights into past herbivore densities. Additionally, this study discusses various factors influencing the composition of the spores of coprophilous fungi, and the abundance of <em>Sporormiella</em>, potential constraints on their preservation in certain settings, and the limitations of current research. This research review article also outlines broader implications and directions for the future research.</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"344 ","pages":"Article 105466"},"PeriodicalIF":1.7,"publicationDate":"2025-11-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145465450","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}