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The Cavern Club Beatles are the Cavern’s resident Beatles tribute band, who play in the Cavern Live Lounge every weekend!

Formed in Liverpool in 2011, these Northern lads, replicate perfectly both the look and sound of the fab four. Their attention to detail, musically and creatively is second to none. The band was cast after extensive auditions “with a little help from” legendary Beatles recording engineer, the late, great Geoff Emerick.

As the officially Cavern endorsed Beatle band, they play their “all – era” theatre style show every Saturday in the Cavern Live Lounge as well a more relaxed show on certain Fridays throughout the year. Please see listing for “Friday With The Cavern Club Beatles”.

Between them they have already notched up an impressive biography – touring the world extensively as well as shows on London’s West End, Broadway, and played The Royal Albert Hall. In February 2014 the band celebrated the 50th Anniversary of the Beatles’ first steps on American soil and their first appearance on the Ed Sullivan show. Over a two – week period they played throughout New York and Florida in conjunction with The City Of Liverpool, Hard Rock Cafe, British Airways and Visit Britain. In 2015 the band were invited to celebrate the 50th Anniversary of the filming of the Beatles’ second film, Help!, in Obertauen, Austria. They performed in Obertauen as well as sold out shows in Vienna. In June of 2016, the band headlined International Beatleweek, performed solo George and Paul shows, as well as a special show to Revolver.

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A Paleosol on a Pre-Cambrian Ferruginous Quartzite Weathering Crust (Stary Oskol, Belgorod Region, Russia)

• Published: 12 March 2022
• Volume 55 , pages 1476–1490, ( 2021 )

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• T. V. Alekseeva 1 ,
• A. O. Alekseev 1 &
• G. V. Mitenko 1  

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This study describes the results of a detailed study (morphology, XRD, Mössbauer and FTIR- spectroscopies, SEM-EDS) of paleosol (PS) developed at the surface of Pre-Cambrian weathering crust of ferruginous quartzite (Kursk Magnetic Anomaly Region). The age of soil formation is estimated as pre-Eifelian. Being developed from pyrite bearing metamorphic rock, the PS includes the characteristics of several pedogenic units, mostly Lithosol and acid sulphate soil. Its specific feature is intensive pedogenesis within the rock at a depth of 10–15 cm, and negligible at the surface. The PS was developed under low monotypic vegetation cover. The sub-micromorphology of plant fragments shows that they belong to either primitive Lycopodiophyta or to Propteridophyta . The similarity between the micromorphology of fragments of surface and subsurface parts of plants shows the development of primitive roots. Azonality of soil characteristics makes paleoclimate reconstructions difficult. For instance, evidence of deep mineral weathering, such as quartz and hematite dissolution, the formation of kaolinite, and amorphous Si, Al, Fe mineral crusts development may reflect climate humidity or aggressive weathering caused by sulfide oxidation. The newly formed gypsum could be a product of deep pyrite oxidation rather than accumulation due to climate aridity. However, its preservation suggests non-humid (semi-arid), rather than humid environments.

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ACKNOWLEDGMENTS

The authors are grateful to the management and geological service of the Stoilensky GOK quarry (NLMK group of companies) for facilitating fieldwork.

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Institute of Physical Chemical and Biological Problems of Soil Science, Russian Academy of Sciences, 142290, Pushchino, Moscow oblast, Russia

T. V. Alekseeva, A. O. Alekseev & G. V. Mitenko

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Correspondence to T. V. Alekseeva .

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Translated by S. Nikolaeva

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Alekseeva, T.V., Alekseev, A.O. & Mitenko, G.V. A Paleosol on a Pre-Cambrian Ferruginous Quartzite Weathering Crust (Stary Oskol, Belgorod Region, Russia). Paleontol. J. 55 , 1476–1490 (2021). https://doi.org/10.1134/S0031030121120054

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Received : 12 April 2021

Revised : 21 June 2021

Accepted : 21 June 2021

Published : 12 March 2022

Issue Date : December 2021

DOI : https://doi.org/10.1134/S0031030121120054

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