首页> 外文期刊>Earth sciences history: Journal of the History of the Earth Sciences Society >EBENEZER EMMONS (1799-1863), FOUNDER OF AMERICAN PALEOZOIC STRATIGRAPHY: HERO OF THE TACONIC CONTROVERSY, ONE OF THE MOST CELEBRATED GEOLOGICAL DISPUTES IN NORTH AMERICA
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EBENEZER EMMONS (1799-1863), FOUNDER OF AMERICAN PALEOZOIC STRATIGRAPHY: HERO OF THE TACONIC CONTROVERSY, ONE OF THE MOST CELEBRATED GEOLOGICAL DISPUTES IN NORTH AMERICA

机译:埃伯尼泽·埃蒙斯(1799-1863),美国古生代地层学的奠基人:泰康争论的英雄,北美洲最著名的地质纠纷之一

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One of the most important and distinguished geologists in the history of the earth sciences was Ebenezer Emmons Sr., father of the Taconie System. The overthrust which places Lower Cumbrian rocks in sill contact with Middle Ordovician rocks, known as Emmons' Line, formerly Logan's Line, is a segment that extends from Canada through New York, and as far south as Alabama. Emmons, a graduate of Rensselaer in the first class of 1826, was inspired by Amos Eaton. Emmons became junior professor at Rensselaer in 1830, a position he held for ten years, and while serving there, was appointed State (Chief) Geologist of the northern Geological District of the New York Earth Sciences History, State Geological Survey in 1S36. He named the Adirondack Mountains (1838), and the Taconie Mountains (1844, 1846) and acquainted the public with these regions. Emmons had noted the presence of a group of rocks between the Potsdam Sandstone, the oldest of the then recognized sedimentary formations in New York, and what was called then the Primitive Rocks of Central Vermont. Emmons inferred that the deformed rocks in Washington County, New York, north of Troy, New York, were older than any fossil iferous rocks then known. For these oldest fossil-bearing rocks he coined the name Taconie System. Emmons later became state geologist of North Carolina, spreading the influence of Rensselaer, and promoted his ideas of the Taconie System.Emmons' student at Rensselaer, James Hall became the chief American paleontologist of his era and one of the greatest American scientists of the 19"1 century. Emmons and Hall 'dueled' over the age of the Taconie rocks, a disagreement that became known as the Taconie controversy. Hall said they were younger, whereas Emmons claimed them to be older. This division led to suit and counter suit, and ultimately Emmons was forced to leave New York as a result of a court decision favoring Hall. Emmons and Hall are buried next to each other at the Albany Rural Cemetery in Albany, New York. The argument over the Taconie fossils raged for many years, and ultimately Emmons was vindicated, for Joachim Barrande, the chief student of European Paleozoic faunas, agreed with Emmons. The Taconie rocks of Troy, New York, arc comparable in age and lithology to the rocks of the district near Prague which have been named Barrandian after Barrande. The American Museum of Natural History in New York honors "Scientists Who Have Served the State of New York and the Nation"; this list includes four geologists, three of whom are from Rensselaer. The first listed is Eaton, founder of Rensselaer, and last is Ebenezer Emmons.
机译:Taconie系统之父Ebenezer Emmons Sr.是地球科学史上最重要和最杰出的地质学家之一。将下坎布里亚岩与奥陶系中段岩石保持基岩接触的推力,该段被称为艾蒙斯线(原称洛根线),从加拿大延伸到纽约,一直延伸到南至阿拉巴马州。艾蒙斯(Emmons)是伦斯勒(Rensselaer)1826年第一届的毕业生,他受到阿莫斯·伊顿(Amos Eaton)的启发。艾蒙斯(Emmons)于1830年在伦斯勒(Rensselaer)担任初级教授,担任该职位十年,在任职期间,他被任命为纽约地球科学史北部地质区的州(首席)地质学家,并于1S36年被任命为州地质调查局。他将阿迪朗达克山脉(1838)和塔科涅山脉(1844,1846)命名,并使公众熟悉这些地区。埃蒙斯(Emmons)注意到波茨坦砂岩(当时纽约当时公认的最古老的沉积岩层)与所谓的佛蒙特中部原始岩之间存在着一组岩石。艾蒙斯(Emmons)推断,纽约特洛伊以北的纽约华盛顿县的变形岩石比当时已知的任何化石铁质岩石都要老。对于这些最古老的含化石的岩石,他创造了Taconie System这个名字。埃蒙斯后来成为北卡罗莱纳州的州地质学家,传播了伦斯勒的影响力,并推广了他对Taconie系统的想法。詹姆斯·霍尔在埃姆斯在伦斯勒的学生中成为了当时的美国首席古生物学家,也是19世纪19年代最伟大的美国科学家之一“ 1世纪。在塔科涅岩石的年代,埃蒙斯和霍尔“决斗”,这一分歧被称为“塔科涅”争议。霍尔说他们年轻,而埃蒙斯声称他们年纪大。这种分歧导致了诉讼和反诉讼,最终法院判决赞成埃蒙斯(Emmons)迫使霍尔离开纽约,埃蒙斯(Emmons)和霍尔被埋葬在纽约奥尔巴尼(Albany)的奥尔巴尼农村公墓中。欧洲古生代动物学的首席学生约阿希姆·巴兰德(Joachim Barrande)同意了埃蒙斯的观点,最终使埃蒙斯得到了证明。纽约特洛伊的Taconie岩石的年龄和岩性与岩石相当布拉格附近的地区,以Barrande的名字命名为Barrandian。纽约美国自然历史博物馆表彰“曾为纽约州和国家服务的科学家”;该清单包括四位地质学家,其中三位来自伦斯勒。首先列出的是Rensselaer的创始人Eaton,最后列出的是Ebenezer Emmons。

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