Reconstruction of a Ross lost Cambrian Series 2mixed siliciclastic–carbonate platform from carbonate clasts of the Shackleton Range, Antarctica

ABSTRACT The presence of archaeocyath-bearing clasts from Cenozoic tills and Cambrian Mount Wegener Formation reveal erosion of a hidden Cambrian carbonate platform in Shackleton Range, Antarctica. We provide microfacies, paleontological, diagenetic and tectonically induced fabric data from carbonat...

Full description

Bibliographic Details
Published in:Earth and Environmental Science Transactions of the Royal Society of Edinburgh
Main Authors: RODRÍGUEZ-MARTÍNEZ, Marta, BUGGISCH, Werner, MENÉNDEZ, Silvia, MORENO-EIRIS, Elena, PEREJÓN, Antonio
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2022
Subjects:
Online Access:http://dx.doi.org/10.1017/s1755691022000111
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S1755691022000111
id crcambridgeupr:10.1017/s1755691022000111
record_format openpolar
spelling crcambridgeupr:10.1017/s1755691022000111 2024-09-15T17:46:07+00:00 Reconstruction of a Ross lost Cambrian Series 2mixed siliciclastic–carbonate platform from carbonate clasts of the Shackleton Range, Antarctica RODRÍGUEZ-MARTÍNEZ, Marta BUGGISCH, Werner MENÉNDEZ, Silvia MORENO-EIRIS, Elena PEREJÓN, Antonio 2022 http://dx.doi.org/10.1017/s1755691022000111 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S1755691022000111 en eng Cambridge University Press (CUP) https://creativecommons.org/licenses/by/4.0/ Earth and Environmental Science Transactions of the Royal Society of Edinburgh volume 113, issue 3, page 175-226 ISSN 1755-6910 1755-6929 journal-article 2022 crcambridgeupr https://doi.org/10.1017/s1755691022000111 2024-07-31T04:04:36Z ABSTRACT The presence of archaeocyath-bearing clasts from Cenozoic tills and Cambrian Mount Wegener Formation reveal erosion of a hidden Cambrian carbonate platform in Shackleton Range, Antarctica. We provide microfacies, paleontological, diagenetic and tectonically induced fabric data from carbonate clasts which, in addition to available geochemical and geochronological data from Shackleton Range, allow the paleoenvironmental reconstruction of a lost Cambrian Series 2 mixed siliciclastic–carbonate platform that was developed and eroded during the Ross orogeny. Carbonate production was dominated by non-skeletal grains in possibly restricted platform-interior and oolitic shoal complex settings, while open subtidal sub-environments (calcimicrobe carpets, calcimicrobe–archaeocyath patch reefs, muddy bottoms) were dominated by a diverse calcimicrobe assemblage and/or by secondary to accessory heterozoan assemblage (archaeocyaths and other sponges, chancelloriids, hyoliths, coralomorphs, trilobites, echinoderms). We describe a Botoman assemblage with 34 archaeocyathan species among 12 existing archaeocyathan genera. A new archaeocyath family Shackletoncyathidae is proposed. New species ( Rotundocyathus glacius sp. nov., Buggischicyathus microporus gen. et sp. nov., Paragnaltacyathus hoeflei , Shackletoncyathus buggischi gen. et. sp. nov., Santelmocyathus santelmoi gen. et sp. nov., Wegenercyathus sexangulae gen. et sp. nov.) and Tabulaconus kordae coralomorph are reported from Antarctica for the first time. Archaeocyathan fauna share few species with contemporary fauna of South Australia (9) and even fewer with the Antarctic platforms of the Shackleton Limestone (2) or the Schneider Hills limestone (1). Similarity is greater with Antarctic allochthonous assemblages of Permo-Carboniferous tillites from Ellsworth Mountains (2), Cenozoic deposits from King George Island (4) or Weddell Sea (1). The Shackleton Range lost/hidden platform shows a distinct entity related with its tectonosedimentary evolution, in a possible ... Article in Journal/Newspaper Antarc* Antarctic Antarctica King George Island Weddell Sea Cambridge University Press Earth and Environmental Science Transactions of the Royal Society of Edinburgh 1 52
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description ABSTRACT The presence of archaeocyath-bearing clasts from Cenozoic tills and Cambrian Mount Wegener Formation reveal erosion of a hidden Cambrian carbonate platform in Shackleton Range, Antarctica. We provide microfacies, paleontological, diagenetic and tectonically induced fabric data from carbonate clasts which, in addition to available geochemical and geochronological data from Shackleton Range, allow the paleoenvironmental reconstruction of a lost Cambrian Series 2 mixed siliciclastic–carbonate platform that was developed and eroded during the Ross orogeny. Carbonate production was dominated by non-skeletal grains in possibly restricted platform-interior and oolitic shoal complex settings, while open subtidal sub-environments (calcimicrobe carpets, calcimicrobe–archaeocyath patch reefs, muddy bottoms) were dominated by a diverse calcimicrobe assemblage and/or by secondary to accessory heterozoan assemblage (archaeocyaths and other sponges, chancelloriids, hyoliths, coralomorphs, trilobites, echinoderms). We describe a Botoman assemblage with 34 archaeocyathan species among 12 existing archaeocyathan genera. A new archaeocyath family Shackletoncyathidae is proposed. New species ( Rotundocyathus glacius sp. nov., Buggischicyathus microporus gen. et sp. nov., Paragnaltacyathus hoeflei , Shackletoncyathus buggischi gen. et. sp. nov., Santelmocyathus santelmoi gen. et sp. nov., Wegenercyathus sexangulae gen. et sp. nov.) and Tabulaconus kordae coralomorph are reported from Antarctica for the first time. Archaeocyathan fauna share few species with contemporary fauna of South Australia (9) and even fewer with the Antarctic platforms of the Shackleton Limestone (2) or the Schneider Hills limestone (1). Similarity is greater with Antarctic allochthonous assemblages of Permo-Carboniferous tillites from Ellsworth Mountains (2), Cenozoic deposits from King George Island (4) or Weddell Sea (1). The Shackleton Range lost/hidden platform shows a distinct entity related with its tectonosedimentary evolution, in a possible ...
format Article in Journal/Newspaper
author RODRÍGUEZ-MARTÍNEZ, Marta
BUGGISCH, Werner
MENÉNDEZ, Silvia
MORENO-EIRIS, Elena
PEREJÓN, Antonio
spellingShingle RODRÍGUEZ-MARTÍNEZ, Marta
BUGGISCH, Werner
MENÉNDEZ, Silvia
MORENO-EIRIS, Elena
PEREJÓN, Antonio
Reconstruction of a Ross lost Cambrian Series 2mixed siliciclastic–carbonate platform from carbonate clasts of the Shackleton Range, Antarctica
author_facet RODRÍGUEZ-MARTÍNEZ, Marta
BUGGISCH, Werner
MENÉNDEZ, Silvia
MORENO-EIRIS, Elena
PEREJÓN, Antonio
author_sort RODRÍGUEZ-MARTÍNEZ, Marta
title Reconstruction of a Ross lost Cambrian Series 2mixed siliciclastic–carbonate platform from carbonate clasts of the Shackleton Range, Antarctica
title_short Reconstruction of a Ross lost Cambrian Series 2mixed siliciclastic–carbonate platform from carbonate clasts of the Shackleton Range, Antarctica
title_full Reconstruction of a Ross lost Cambrian Series 2mixed siliciclastic–carbonate platform from carbonate clasts of the Shackleton Range, Antarctica
title_fullStr Reconstruction of a Ross lost Cambrian Series 2mixed siliciclastic–carbonate platform from carbonate clasts of the Shackleton Range, Antarctica
title_full_unstemmed Reconstruction of a Ross lost Cambrian Series 2mixed siliciclastic–carbonate platform from carbonate clasts of the Shackleton Range, Antarctica
title_sort reconstruction of a ross lost cambrian series 2mixed siliciclastic–carbonate platform from carbonate clasts of the shackleton range, antarctica
publisher Cambridge University Press (CUP)
publishDate 2022
url http://dx.doi.org/10.1017/s1755691022000111
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S1755691022000111
genre Antarc*
Antarctic
Antarctica
King George Island
Weddell Sea
genre_facet Antarc*
Antarctic
Antarctica
King George Island
Weddell Sea
op_source Earth and Environmental Science Transactions of the Royal Society of Edinburgh
volume 113, issue 3, page 175-226
ISSN 1755-6910 1755-6929
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/s1755691022000111
container_title Earth and Environmental Science Transactions of the Royal Society of Edinburgh
container_start_page 1
op_container_end_page 52
_version_ 1810494095709175808