Chemical taphonomy and preservation modes of Jurassic spinicaudatans from Patagonia: A chemometric approach
Spinicaudatans ('clam shrimps') are small branchiopod crustaceans enclosed in a chitinous bivalved carapace that is often the only preserved element in the fossil record. However, few studies have analyzed the preservation of these carapaces, which have been found in continental facies fro...
Guardado en:
| Publicado: |
2018
|
|---|---|
| Materias: | |
| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00223360_v92_n6_p1054_Monferran http://hdl.handle.net/20.500.12110/paper_00223360_v92_n6_p1054_Monferran |
| Aporte de: |
| id |
paper:paper_00223360_v92_n6_p1054_Monferran |
|---|---|
| record_format |
dspace |
| spelling |
paper:paper_00223360_v92_n6_p1054_Monferran2023-06-08T14:49:51Z Chemical taphonomy and preservation modes of Jurassic spinicaudatans from Patagonia: A chemometric approach bivalve chemical analysis crustacean Devonian diagenesis facies fossil record Jurassic ornamentation preservation recrystallization taphonomy Argentina Patagonia Branchiopoda Conchostraca Crustacea Spinicaudatans ('clam shrimps') are small branchiopod crustaceans enclosed in a chitinous bivalved carapace that is often the only preserved element in the fossil record. However, few studies have analyzed the preservation of these carapaces, which have been found in continental facies from the Devonian to the present. The aim of this study was to contribute to a better understanding of the chemical preservation of fossil spinicaudatan carapaces, and it focused on spinicaudatan carapaces of the Cañadón Asfalto Formation from the Jurassic of Argentina. Semiquantitative energy-dispersive X-ray spectrometry (EDS) analysis provided elemental composition data that were interpreted using principal component analysis (PCA). The results showed a complex chemical mode of preservation for spinicaudatan carapaces. In some parts, EDS spectra of the specimens exhibit peaks of calcium, phosphorous, aluminum, and fluorine, representing the retention of original carapace material with some diagenetic recrystallization. Certain zones of the carapace show low-intensity peaks of the elements mentioned, while silicon and oxygen peaks (from the rock matrix) become the dominant spectral signals. These modes of preservation modify the interpretations and observations of the ornamentation of the carapace, which are used as taxonomic features. Our results suggest that specific diagenetic processes play a fundamental role in the preservation of spinicaudatans. © 2018, The Paleontological Society. 2018 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00223360_v92_n6_p1054_Monferran http://hdl.handle.net/20.500.12110/paper_00223360_v92_n6_p1054_Monferran |
| institution |
Universidad de Buenos Aires |
| institution_str |
I-28 |
| repository_str |
R-134 |
| collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
| topic |
bivalve chemical analysis crustacean Devonian diagenesis facies fossil record Jurassic ornamentation preservation recrystallization taphonomy Argentina Patagonia Branchiopoda Conchostraca Crustacea |
| spellingShingle |
bivalve chemical analysis crustacean Devonian diagenesis facies fossil record Jurassic ornamentation preservation recrystallization taphonomy Argentina Patagonia Branchiopoda Conchostraca Crustacea Chemical taphonomy and preservation modes of Jurassic spinicaudatans from Patagonia: A chemometric approach |
| topic_facet |
bivalve chemical analysis crustacean Devonian diagenesis facies fossil record Jurassic ornamentation preservation recrystallization taphonomy Argentina Patagonia Branchiopoda Conchostraca Crustacea |
| description |
Spinicaudatans ('clam shrimps') are small branchiopod crustaceans enclosed in a chitinous bivalved carapace that is often the only preserved element in the fossil record. However, few studies have analyzed the preservation of these carapaces, which have been found in continental facies from the Devonian to the present. The aim of this study was to contribute to a better understanding of the chemical preservation of fossil spinicaudatan carapaces, and it focused on spinicaudatan carapaces of the Cañadón Asfalto Formation from the Jurassic of Argentina. Semiquantitative energy-dispersive X-ray spectrometry (EDS) analysis provided elemental composition data that were interpreted using principal component analysis (PCA). The results showed a complex chemical mode of preservation for spinicaudatan carapaces. In some parts, EDS spectra of the specimens exhibit peaks of calcium, phosphorous, aluminum, and fluorine, representing the retention of original carapace material with some diagenetic recrystallization. Certain zones of the carapace show low-intensity peaks of the elements mentioned, while silicon and oxygen peaks (from the rock matrix) become the dominant spectral signals. These modes of preservation modify the interpretations and observations of the ornamentation of the carapace, which are used as taxonomic features. Our results suggest that specific diagenetic processes play a fundamental role in the preservation of spinicaudatans. © 2018, The Paleontological Society. |
| title |
Chemical taphonomy and preservation modes of Jurassic spinicaudatans from Patagonia: A chemometric approach |
| title_short |
Chemical taphonomy and preservation modes of Jurassic spinicaudatans from Patagonia: A chemometric approach |
| title_full |
Chemical taphonomy and preservation modes of Jurassic spinicaudatans from Patagonia: A chemometric approach |
| title_fullStr |
Chemical taphonomy and preservation modes of Jurassic spinicaudatans from Patagonia: A chemometric approach |
| title_full_unstemmed |
Chemical taphonomy and preservation modes of Jurassic spinicaudatans from Patagonia: A chemometric approach |
| title_sort |
chemical taphonomy and preservation modes of jurassic spinicaudatans from patagonia: a chemometric approach |
| publishDate |
2018 |
| url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00223360_v92_n6_p1054_Monferran http://hdl.handle.net/20.500.12110/paper_00223360_v92_n6_p1054_Monferran |
| _version_ |
1768544988882272256 |