Michael H. Stephenson , Shuzhong Shen , Junxuan Fan , Linshu Hu , Jin Qi
{"title":"陡峭的气候梯度对两个石炭纪-二叠纪冰期片中特提斯海岸阿拉伯部分孢粉组合的影响","authors":"Michael H. Stephenson , Shuzhong Shen , Junxuan Fan , Linshu Hu , Jin Qi","doi":"10.1016/j.revpalbo.2025.105448","DOIUrl":null,"url":null,"abstract":"<div><div>Palaeoclimate modelling of two time slices, Serpukhovian to Bashkirian (Carboniferous), and Gzhelian to early Sakmarian (latest Carboniferous to Early Permian), indicates marked changes in palynological assemblages from 30°S and 50°S across the Gondwana and Tethys margin. Both time slices indicate a distinct cold climate assemblage dominated by cheilocardioid spores, while a warmer climate with mean annual temperature above 19 °C appears to encourage the growth of plants that produced Euramerican coal belt spores such as <em>Vestispora fenestrata</em> and <em>Reticulatisporites polygonalis</em>. It is possible that the parent plants of cingulicamerate spores such as <em>Lundbladispora</em> spp., though tolerant of cold conditions, were not tolerant of the coldest conditions (for example below 0 °C).</div></div>","PeriodicalId":54488,"journal":{"name":"Review of Palaeobotany and Palynology","volume":"344 ","pages":"Article 105448"},"PeriodicalIF":1.7000,"publicationDate":"2025-09-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Effect of steep climate gradient on palynological assemblages on the Arabian part of the Tethys shore in two Carboniferous-Permian ice age time slices\",\"authors\":\"Michael H. Stephenson , Shuzhong Shen , Junxuan Fan , Linshu Hu , Jin Qi\",\"doi\":\"10.1016/j.revpalbo.2025.105448\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Palaeoclimate modelling of two time slices, Serpukhovian to Bashkirian (Carboniferous), and Gzhelian to early Sakmarian (latest Carboniferous to Early Permian), indicates marked changes in palynological assemblages from 30°S and 50°S across the Gondwana and Tethys margin. Both time slices indicate a distinct cold climate assemblage dominated by cheilocardioid spores, while a warmer climate with mean annual temperature above 19 °C appears to encourage the growth of plants that produced Euramerican coal belt spores such as <em>Vestispora fenestrata</em> and <em>Reticulatisporites polygonalis</em>. It is possible that the parent plants of cingulicamerate spores such as <em>Lundbladispora</em> spp., though tolerant of cold conditions, were not tolerant of the coldest conditions (for example below 0 °C).</div></div>\",\"PeriodicalId\":54488,\"journal\":{\"name\":\"Review of Palaeobotany and Palynology\",\"volume\":\"344 \",\"pages\":\"Article 105448\"},\"PeriodicalIF\":1.7000,\"publicationDate\":\"2025-09-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Review of Palaeobotany and Palynology\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0034666725001691\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"PALEONTOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Review of Palaeobotany and Palynology","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0034666725001691","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"PALEONTOLOGY","Score":null,"Total":0}
Effect of steep climate gradient on palynological assemblages on the Arabian part of the Tethys shore in two Carboniferous-Permian ice age time slices
Palaeoclimate modelling of two time slices, Serpukhovian to Bashkirian (Carboniferous), and Gzhelian to early Sakmarian (latest Carboniferous to Early Permian), indicates marked changes in palynological assemblages from 30°S and 50°S across the Gondwana and Tethys margin. Both time slices indicate a distinct cold climate assemblage dominated by cheilocardioid spores, while a warmer climate with mean annual temperature above 19 °C appears to encourage the growth of plants that produced Euramerican coal belt spores such as Vestispora fenestrata and Reticulatisporites polygonalis. It is possible that the parent plants of cingulicamerate spores such as Lundbladispora spp., though tolerant of cold conditions, were not tolerant of the coldest conditions (for example below 0 °C).
期刊介绍:
The Review of Palaeobotany and Palynology is an international journal for articles in all fields of palaeobotany and palynology dealing with all groups, ranging from marine palynomorphs to higher land plants. Original contributions and comprehensive review papers should appeal to an international audience. Typical topics include but are not restricted to systematics, evolution, palaeobiology, palaeoecology, biostratigraphy, biochronology, palaeoclimatology, paleogeography, taphonomy, palaeoenvironmental reconstructions, vegetation history, and practical applications of palaeobotany and palynology, e.g. in coal and petroleum geology and archaeology. The journal especially encourages the publication of articles in which palaeobotany and palynology are applied for solving fundamental geological and biological problems as well as innovative and interdisciplinary approaches.