{"title":"牙形刺在时间和空间上的大小:超越温度大小规则","authors":"Catherine Girard , Anne-Lise Charruault , Anne-Béatrice Dufour , Sabrina Renaud","doi":"10.1016/j.marmicro.2023.102291","DOIUrl":null,"url":null,"abstract":"<div><p><span>The temperature-size rule (TSR) states that ectotherms mature at smaller adult body size in warmer conditions. Such a rule may have the potential to explain size response of fossil<span> organisms to past temperature variations, but its validity in deep time has been seldom tested. The generality of this rule was investigated here by compiling data documenting the size record of three conodont genera (</span></span><em>Palmatolepis, Ancyrodella</em> and <em>Polygnathus</em><span><span>) at different spatial and temporal scales during the Late Frasnian<span> and the Famennian, characterized by short- and long-term temperature variations. Statistical models were used to investigate the relationship between conodont size and </span></span>oxygen isotope<span> values, considered as paleotemperature proxies. Comparison of evolutionary models further allowed to test alternative modes of size variation such as stasis or punctuation.</span></span></p><p>The TSR was not validated as a general rule explaining size variation in these fossil records, being only observed as a large-scale geographic trend during a time-slice. The only strong support for temperature being the driver of temporal variations was found regarding the size of <em>Palmatolepis</em> during the Kellwasser period, but the relationship was reverse to the expectation of the TSR. The absence of general TSR pattern is probably due to the interference of many other factors (demography and mortality patterns, temperature tolerance, size reduction due to stress) whose relative importance may depend on the time interval and the genus considered. Rather than a correlation with environmental proxies, evolutionary models suggested the occurrence of a synchronous shift in <em>Palmatolepis</em> size around 369 Ma (<em>Palmatolepis termini</em> conodont Zone) in several outcrops, raising questions about the environmental forcing beyond this shift. Departures from the expected TSR may thus provide relevant insights into the complex interplay of physical, tectonic and eco-evolutionary processes impacting size evolution in deep time.</p></div>","PeriodicalId":49881,"journal":{"name":"Marine Micropaleontology","volume":"184 ","pages":"Article 102291"},"PeriodicalIF":1.5000,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Conodont size in time and space: Beyond the temperature-size rule\",\"authors\":\"Catherine Girard , Anne-Lise Charruault , Anne-Béatrice Dufour , Sabrina Renaud\",\"doi\":\"10.1016/j.marmicro.2023.102291\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p><span>The temperature-size rule (TSR) states that ectotherms mature at smaller adult body size in warmer conditions. Such a rule may have the potential to explain size response of fossil<span> organisms to past temperature variations, but its validity in deep time has been seldom tested. The generality of this rule was investigated here by compiling data documenting the size record of three conodont genera (</span></span><em>Palmatolepis, Ancyrodella</em> and <em>Polygnathus</em><span><span>) at different spatial and temporal scales during the Late Frasnian<span> and the Famennian, characterized by short- and long-term temperature variations. Statistical models were used to investigate the relationship between conodont size and </span></span>oxygen isotope<span> values, considered as paleotemperature proxies. Comparison of evolutionary models further allowed to test alternative modes of size variation such as stasis or punctuation.</span></span></p><p>The TSR was not validated as a general rule explaining size variation in these fossil records, being only observed as a large-scale geographic trend during a time-slice. The only strong support for temperature being the driver of temporal variations was found regarding the size of <em>Palmatolepis</em> during the Kellwasser period, but the relationship was reverse to the expectation of the TSR. The absence of general TSR pattern is probably due to the interference of many other factors (demography and mortality patterns, temperature tolerance, size reduction due to stress) whose relative importance may depend on the time interval and the genus considered. Rather than a correlation with environmental proxies, evolutionary models suggested the occurrence of a synchronous shift in <em>Palmatolepis</em> size around 369 Ma (<em>Palmatolepis termini</em> conodont Zone) in several outcrops, raising questions about the environmental forcing beyond this shift. Departures from the expected TSR may thus provide relevant insights into the complex interplay of physical, tectonic and eco-evolutionary processes impacting size evolution in deep time.</p></div>\",\"PeriodicalId\":49881,\"journal\":{\"name\":\"Marine Micropaleontology\",\"volume\":\"184 \",\"pages\":\"Article 102291\"},\"PeriodicalIF\":1.5000,\"publicationDate\":\"2023-09-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Marine Micropaleontology\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0377839823000907\",\"RegionNum\":4,\"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":"Marine Micropaleontology","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0377839823000907","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"PALEONTOLOGY","Score":null,"Total":0}
引用次数: 0
摘要
温度尺寸规则(TSR)指出,在温暖的条件下,变温动物成年时的体型较小。这样的规则可能有潜力解释化石生物对过去温度变化的大小反应,但其在深时间的有效性很少得到检验。本文通过整理三种牙形刺属(Palmatolepis、Ancyrodella和Polygnathus)在晚弗拉斯纪和法门纪不同时空尺度上的尺寸记录,以短期和长期温度变化为特征,探讨了这一规律的普遍性。采用统计模型研究牙形石大小与氧同位素值之间的关系,并将其作为古温标。进化模型的比较进一步允许测试大小变化的替代模式,如停滞或标点符号。TSR并没有被证实为解释这些化石记录中大小变化的一般规则,只是在一个时间片中作为一个大尺度的地理趋势被观察到。在Kellwasser时期,Palmatolepis的大小对温度是时间变化的驱动因素提供了唯一强有力的支持,但与TSR的期望相反。一般TSR模式的缺失可能是由于许多其他因素的干扰(人口和死亡率模式,温度耐受性,由于胁迫而导致的尺寸缩小),其相对重要性可能取决于所考虑的时间间隔和属。进化模型表明,在369 Ma (Palmatolepis termini牙形带)的几个露头中,Palmatolepis的大小发生了同步变化,而不是与环境代用物的相关性,这引发了关于这种变化之外的环境强迫的问题。因此,与预期TSR的偏离可能为深入了解影响尺寸演化的物理、构造和生态演化过程的复杂相互作用提供相关见解。
Conodont size in time and space: Beyond the temperature-size rule
The temperature-size rule (TSR) states that ectotherms mature at smaller adult body size in warmer conditions. Such a rule may have the potential to explain size response of fossil organisms to past temperature variations, but its validity in deep time has been seldom tested. The generality of this rule was investigated here by compiling data documenting the size record of three conodont genera (Palmatolepis, Ancyrodella and Polygnathus) at different spatial and temporal scales during the Late Frasnian and the Famennian, characterized by short- and long-term temperature variations. Statistical models were used to investigate the relationship between conodont size and oxygen isotope values, considered as paleotemperature proxies. Comparison of evolutionary models further allowed to test alternative modes of size variation such as stasis or punctuation.
The TSR was not validated as a general rule explaining size variation in these fossil records, being only observed as a large-scale geographic trend during a time-slice. The only strong support for temperature being the driver of temporal variations was found regarding the size of Palmatolepis during the Kellwasser period, but the relationship was reverse to the expectation of the TSR. The absence of general TSR pattern is probably due to the interference of many other factors (demography and mortality patterns, temperature tolerance, size reduction due to stress) whose relative importance may depend on the time interval and the genus considered. Rather than a correlation with environmental proxies, evolutionary models suggested the occurrence of a synchronous shift in Palmatolepis size around 369 Ma (Palmatolepis termini conodont Zone) in several outcrops, raising questions about the environmental forcing beyond this shift. Departures from the expected TSR may thus provide relevant insights into the complex interplay of physical, tectonic and eco-evolutionary processes impacting size evolution in deep time.
期刊介绍:
Marine Micropaleontology is an international journal publishing original, innovative and significant scientific papers in all fields related to marine microfossils, including ecology and paleoecology, biology and paleobiology, paleoceanography and paleoclimatology, environmental monitoring, taphonomy, evolution and molecular phylogeny. The journal strongly encourages the publication of articles in which marine microfossils and/or their chemical composition are used to solve fundamental geological, environmental and biological problems. However, it does not publish purely stratigraphic or taxonomic papers. In Marine Micropaleontology, a special section is dedicated to short papers on new methods and protocols using marine microfossils. We solicit special issues on hot topics in marine micropaleontology and review articles on timely subjects.