{"title":"讨论“罗伯特·詹姆森在爱丁堡大学的演讲中所反映的从海王星到钚的转变,1820–33”:《苏格兰地质学杂志》,56,85–99,https://doi.org/10.1144/sjg2019-031","authors":"J. Gordon","doi":"10.1144/sjg2020-022","DOIUrl":null,"url":null,"abstract":"In his illuminating review of the progress of Robert Jameson’s conversion from Neptunism (promoted by Abraham Werner) to Plutonism (developed from the ideas of James Hutton), Stone (2020) drew extensively on the extant lecture notes taken by some of Jameson’s students between about 1820 and 1833. Mention was made in passing of Jameson’s role as an early proponent of Scottish glaciation, but the secondary literature sources cited have their primary origin in the notes of another of Jameson’s students, James David Forbes (1809–68), which are now held in the Special Collections of the University of St Andrews Library but were not utilized by Stone. James Forbes – not to be confused with the eminent marine biologist, Edward Forbes (1815–54), who succeeded Jameson to the chair of Natural History at the University of Edinburgh in 1854 – was, in the words of his biographer, Frank Cunningham (1990), a ‘pioneer Scottish glaciologist’. Forbes attended Jameson’s lecture course in Natural History at the University of Edinburgh in session 1827–28 and repeated the class in 1828–29. Forbes’ notes provide a valuable complement to those cited by Stone. Cunningham (1990, p. 14) records that, on the basis of Forbes’ notes, Jameson ‘treated his students to a thoroughly Wernerian version of geology’. Forbes’ notes also provide additional constraint to the timing deduced by Stone for Jameson’s conversion; he was a thoroughly Wernerian Neptunist in 1828 but a convert to Plutonism by 1830. With regard to glaciation, Forbes records in his notes from Jameson’s lecture 12 on 27 November 1827:","PeriodicalId":49556,"journal":{"name":"Scottish Journal of Geology","volume":" ","pages":""},"PeriodicalIF":0.5000,"publicationDate":"2020-11-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1144/sjg2020-022","citationCount":"0","resultStr":"{\"title\":\"Discussion on ‘Robert Jameson's transition from Neptunism to Plutonism as reflected in his lectures at Edinburgh University, 1820–33’: Scottish Journal of Geology, 56, 85–99, https://doi.org/10.1144/sjg2019-031\",\"authors\":\"J. Gordon\",\"doi\":\"10.1144/sjg2020-022\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In his illuminating review of the progress of Robert Jameson’s conversion from Neptunism (promoted by Abraham Werner) to Plutonism (developed from the ideas of James Hutton), Stone (2020) drew extensively on the extant lecture notes taken by some of Jameson’s students between about 1820 and 1833. Mention was made in passing of Jameson’s role as an early proponent of Scottish glaciation, but the secondary literature sources cited have their primary origin in the notes of another of Jameson’s students, James David Forbes (1809–68), which are now held in the Special Collections of the University of St Andrews Library but were not utilized by Stone. James Forbes – not to be confused with the eminent marine biologist, Edward Forbes (1815–54), who succeeded Jameson to the chair of Natural History at the University of Edinburgh in 1854 – was, in the words of his biographer, Frank Cunningham (1990), a ‘pioneer Scottish glaciologist’. Forbes attended Jameson’s lecture course in Natural History at the University of Edinburgh in session 1827–28 and repeated the class in 1828–29. Forbes’ notes provide a valuable complement to those cited by Stone. Cunningham (1990, p. 14) records that, on the basis of Forbes’ notes, Jameson ‘treated his students to a thoroughly Wernerian version of geology’. Forbes’ notes also provide additional constraint to the timing deduced by Stone for Jameson’s conversion; he was a thoroughly Wernerian Neptunist in 1828 but a convert to Plutonism by 1830. 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Discussion on ‘Robert Jameson's transition from Neptunism to Plutonism as reflected in his lectures at Edinburgh University, 1820–33’: Scottish Journal of Geology, 56, 85–99, https://doi.org/10.1144/sjg2019-031
In his illuminating review of the progress of Robert Jameson’s conversion from Neptunism (promoted by Abraham Werner) to Plutonism (developed from the ideas of James Hutton), Stone (2020) drew extensively on the extant lecture notes taken by some of Jameson’s students between about 1820 and 1833. Mention was made in passing of Jameson’s role as an early proponent of Scottish glaciation, but the secondary literature sources cited have their primary origin in the notes of another of Jameson’s students, James David Forbes (1809–68), which are now held in the Special Collections of the University of St Andrews Library but were not utilized by Stone. James Forbes – not to be confused with the eminent marine biologist, Edward Forbes (1815–54), who succeeded Jameson to the chair of Natural History at the University of Edinburgh in 1854 – was, in the words of his biographer, Frank Cunningham (1990), a ‘pioneer Scottish glaciologist’. Forbes attended Jameson’s lecture course in Natural History at the University of Edinburgh in session 1827–28 and repeated the class in 1828–29. Forbes’ notes provide a valuable complement to those cited by Stone. Cunningham (1990, p. 14) records that, on the basis of Forbes’ notes, Jameson ‘treated his students to a thoroughly Wernerian version of geology’. Forbes’ notes also provide additional constraint to the timing deduced by Stone for Jameson’s conversion; he was a thoroughly Wernerian Neptunist in 1828 but a convert to Plutonism by 1830. With regard to glaciation, Forbes records in his notes from Jameson’s lecture 12 on 27 November 1827:
期刊介绍:
Although published only since 1965, the Scottish Journal of Geology has a long pedigree. It is the joint publication of the Geological Society of Glasgow and the Edinburgh Geological Society, which prior to 1965 published separate Transactions: from 1860 in the case of Glasgow and 1863 for Edinburgh.
Traditionally, the Journal has acted as the focus for papers on all aspects of Scottish geology and its contiguous areas, including the surrounding seas. The publication policy has always been outward looking, with the Editors encouraging review papers and papers on broader aspects of the Earth sciences that cannot be discussed solely in terms of Scottish geology.
The diverse geology of Scotland continues to provide an important natural laboratory for the study of earth sciences; many seminal studies in geology have been carried out on Scottish rocks, and over the years the results of much of this work had been published in the Journal and its predecessors.
The Journal fully deserves its high reputation worldwide and intends to maintain its status in the front rank of publications in the Earth sciences.