Insect Trace Fossil Associations in Paleosols: The Coprinisphaera Ichnofacies
2000; Society for Sedimentary Geology; Volume: 15; Issue: 1 Linguagem: Inglês
10.2307/3515591
ISSN1938-5323
AutoresJorge F. Genise, M. Gabriela Mángano, Luís A. Buatois, José H. Laza, Mariano Verde,
Tópico(s)Geological and Geophysical Studies
ResumoOther| February 01, 2000 Insect Trace Fossil Associations in Paleosols: The Coprinisphaera Ichnofacies JORGE F. GENISE; JORGE F. GENISE 1Conicet-Crilar, 5301 Anillaco, La Rioja, Argentina Search for other works by this author on: GSW Google Scholar M. GABRIELA MáNGANO; M. GABRIELA MáNGANO 2Instituto Superior de Correlación Geológica, Facultad de Ciencias Naturales, Universidad Nacional de Tucumán, Casilla de correo 1 (CC), 4000 San Miguel de Tucumán, Argentina Search for other works by this author on: GSW Google Scholar LUIS A. BUATOIS; LUIS A. BUATOIS 2Instituto Superior de Correlación Geológica, Facultad de Ciencias Naturales, Universidad Nacional de Tucumán, Casilla de correo 1 (CC), 4000 San Miguel de Tucumán, Argentina Search for other works by this author on: GSW Google Scholar JOSÉ H. LAZA; JOSÉ H. LAZA 3Laboratorio de Icnología, Museo Argentino de Ciencias Naturales, Av. Angel Gallardo 470, 1405 Buenos Aires, Argentina Search for other works by this author on: GSW Google Scholar MARIANO VERDE MARIANO VERDE 4Departamento de Paleontología, Facultad de Ciencias, Universidad de la República, Iguá 4225,11400 Montevideo,Uruguay Search for other works by this author on: GSW Google Scholar Author and Article Information JORGE F. GENISE 1Conicet-Crilar, 5301 Anillaco, La Rioja, Argentina M. GABRIELA MáNGANO 2Instituto Superior de Correlación Geológica, Facultad de Ciencias Naturales, Universidad Nacional de Tucumán, Casilla de correo 1 (CC), 4000 San Miguel de Tucumán, Argentina LUIS A. BUATOIS 2Instituto Superior de Correlación Geológica, Facultad de Ciencias Naturales, Universidad Nacional de Tucumán, Casilla de correo 1 (CC), 4000 San Miguel de Tucumán, Argentina JOSÉ H. LAZA 3Laboratorio de Icnología, Museo Argentino de Ciencias Naturales, Av. Angel Gallardo 470, 1405 Buenos Aires, Argentina MARIANO VERDE 4Departamento de Paleontología, Facultad de Ciencias, Universidad de la República, Iguá 4225,11400 Montevideo,Uruguay Publisher: SEPM Society for Sedimentary Geology Accepted: 02 Sep 1999 First Online: 03 Mar 2017 Online ISSN: 1938-5323 Print ISSN: 0883-1351 Society for Sedimentary Geology PALAIOS (2000) 15 (1): 49–64. https://doi.org/10.1669/0883-1351(2000)015 2.0.CO;2 Article history Accepted: 02 Sep 1999 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation JORGE F. GENISE, M. GABRIELA MáNGANO, LUIS A. BUATOIS, JOSÉ H. LAZA, MARIANO VERDE; Insect Trace Fossil Associations in Paleosols: The Coprinisphaera Ichnofacies. PALAIOS 2000;; 15 (1): 49–64. doi: https://doi.org/10.1669/0883-1351(2000)015 2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyPALAIOS Search Advanced Search Abstract Analysis of fifty-eight paleosol trace fossil assemblages, ranging from the Triassic to the Recent, allows refinement of continental ichnofacies models and the proposal of a Coprinisphaera ichnofacies. The Coprinisphaera ichnofacies consists of trace fossils of bees, wasps, ants, beetles, termites, and other unassigned insects. Meniscate burrows, mammal caves, and rhizoliths also may be present. This ichnofacies is named after the dung beetle nest Coprinisphaera, the most common component of this archetypal assemblage. In mature paleosols, the Coprinisphaera ichnofacies has moderate to relatively high trace fossil diversity and high abundance. Ethologically, this assemblage is dominated by nesting traces (calichnia) and exhibits a relatively complex tiering pattern, reflecting variable depths of emplacement of hymenopterous, termite, and dung beetle nests. Common components include the bee cells Celliforma, Uruguay, Ellipsoideichnus, Palmiraichnus, and Rosellichnus; the wasp nest Chubutolithes; the ant traces Attaichnus and Parowanichnus, and other beetle traces, such as Monesichnus, Fontanai, and Teisseirei. Termite nests may occur, but are less common components of the Coprinisphaera ichnofacies.The Coprinisphaera ichnofacies fulfills all the requirements to qualify as a Seilacherian or archetypal ichnofacies, namely recurrence in time and space, and distinct paleoenvironmental implications. Proposal of the Coprinisphaera ichnofacies is based on the analysis of twenty-eight cases, ranging from the? Late Cretaceous to the Recent. The Coprinisphaera chnofacies characterizes paleosols developed in paleoecosystems of herbaceous communities. These herbaceous communities range from dry-and-cold to humid-and-warm climates. More detailed paleoclimatological inferences can be obtained by evaluating the relative abundance of the various traces within the assemblage. A dominance of hymenopterous traces would indicate drier conditions, whereas the presence of termite nests would indicate more humid. The Coprinisphaera ichnofacies occurs in paleosols developed in various depositional systems subject to subaerial exposure, such as alluvial plains, desiccated floodplains, crevasse splays, levees, abandoned point bars, and vegetated eolian environments. This and other potential terrestrial ichnofacies are controlled by ecological parameters (e.g., vegetation, climate, and soil) rather than by depositional processes. The association of fossil insect nests indicates the extent of soil development and, consequently, such ichnofossils are one of the best indicators of paleosols.The previously proposed Termitichnus ichnofacies was defined to include all paleosol trace fossil assemblages. However, the available information indicates that terrestrial environments are far more complex. Therefore, it is suggested that the Termitichnus ichnofacies as presently defined be abandoned because it does not reflect the diversity of paleosol settings and fails to provide significant paleoecologic information. Formal definition of a Termitichnus ichnofacies in a more restricted sense, to include assemblages dominated by termite nests in paleosols of closed forest ecosystems, should await documentation of additional studies to prove recurrence. Other fossil insect-nest associations in paleosols (e.g., halictid nests in calcareous soils) do not have enough recurrence in time and space to be considered Seilacherian ichnofacies, but do represent potential ichnofacies. The model proposed in this paper includes the paleoecologically defined Coprinisphaera ichnofacies plus a definite number of associations, each one possessing its own paleoenvironmental implications, which do not show the necessary recurrence to be considered ichnofacies, at present. Climate and vegetation are considered key factors in the shaping of terrestrial ecosystems and should be taken into account for the definition of additional terrestrial ichnofacies. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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