Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall

Autores
Genise, Jorge Fernando; Farina, Juan Luis; Verde, Mariano
Año de publicación
2013
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The trace fossil Teisseirei barattinia, found in Cenozoic formations of Uruguay and Argentina, is an elongated chamber recognizable by its depressed cross-section, antechamber, and its multi-layered lining with an inner surface texture composed of densely packed sub-rectangular to sub-triangular pits. Our recent behavioural observations on larval and pupal stages of Sphingidae (Lepidoptera), particularly on Manduca rustica, suggest that Teisseirei barattinia is the pupation chamber of a sphinx moth. Last instar larvae of Manduca rustica, Eumorpha anchemolus and E. labruscae were placed in terraria to observe their burrowing behaviour and to recover pupation chambers. Chambers show depressed or plane convex cross-sections as T. barattinia. The internal surface texture of walls is also similar to that of T. barattinia. The same pattern could be obtained experimentally by pressing the true legs of Manduca rustica larva against plasticine. The multi-layered wall structure, shown by T. barattinia, is a new type of lining for insect trace fossils in palaeosols that result from soil packing combined with discharges of abundant liquid excretion by soft-bodied larvae, as in the case of Manduca rustica. T. barattinia is the first trace fossil documented in palaeosols attributed to sphinx moths and supported by macro and micromorphological comparisons with extant pupation chambers. The shallow emplacement of moth pupation chambers in soils suggests that T. barattinia would be a good indicator of palaeosol upper horizons.
Fil: Genise, Jorge Fernando. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales; Argentina. Universidad de la Republica. Facultad de Ciencias;
Fil: Farina, Juan Luis. Provincia de Buenos Aires. Municipalidad de General Pueyrredon. Secretaria de Cultura. Museo Municipal de Cs Naturales Lorenzo Scaglia; Argentina
Fil: Verde, Mariano. Universidad de la República; Uruguay
Materia
MULTI-LAYERED WALL
PALAEOPEDOLOGICAL SIGNIFICANCE
PUPATION CHAMBERS
SPHINX MOTH
TEISSEIREI BARATTINIA
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/1364

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spelling Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wallGenise, Jorge FernandoFarina, Juan LuisVerde, MarianoMULTI-LAYERED WALLPALAEOPEDOLOGICAL SIGNIFICANCEPUPATION CHAMBERSSPHINX MOTHTEISSEIREI BARATTINIAhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The trace fossil Teisseirei barattinia, found in Cenozoic formations of Uruguay and Argentina, is an elongated chamber recognizable by its depressed cross-section, antechamber, and its multi-layered lining with an inner surface texture composed of densely packed sub-rectangular to sub-triangular pits. Our recent behavioural observations on larval and pupal stages of Sphingidae (Lepidoptera), particularly on Manduca rustica, suggest that Teisseirei barattinia is the pupation chamber of a sphinx moth. Last instar larvae of Manduca rustica, Eumorpha anchemolus and E. labruscae were placed in terraria to observe their burrowing behaviour and to recover pupation chambers. Chambers show depressed or plane convex cross-sections as T. barattinia. The internal surface texture of walls is also similar to that of T. barattinia. The same pattern could be obtained experimentally by pressing the true legs of Manduca rustica larva against plasticine. The multi-layered wall structure, shown by T. barattinia, is a new type of lining for insect trace fossils in palaeosols that result from soil packing combined with discharges of abundant liquid excretion by soft-bodied larvae, as in the case of Manduca rustica. T. barattinia is the first trace fossil documented in palaeosols attributed to sphinx moths and supported by macro and micromorphological comparisons with extant pupation chambers. The shallow emplacement of moth pupation chambers in soils suggests that T. barattinia would be a good indicator of palaeosol upper horizons.Fil: Genise, Jorge Fernando. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales; Argentina. Universidad de la Republica. Facultad de Ciencias;Fil: Farina, Juan Luis. Provincia de Buenos Aires. Municipalidad de General Pueyrredon. Secretaria de Cultura. Museo Municipal de Cs Naturales Lorenzo Scaglia; ArgentinaFil: Verde, Mariano. Universidad de la República; UruguayWiley Blackwell Publishing, Inc2013-07info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/1364Genise, Jorge Fernando; Farina, Juan Luis; Verde, Mariano; Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall; Wiley Blackwell Publishing, Inc; Lethaia; 46; 4; 7-2013; 480-4890024-1164enginfo:eu-repo/semantics/altIdentifier/doi/10.1111/let.12025info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-10T13:05:01Zoai:ri.conicet.gov.ar:11336/1364instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-10 13:05:01.972CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall
title Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall
spellingShingle Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall
Genise, Jorge Fernando
MULTI-LAYERED WALL
PALAEOPEDOLOGICAL SIGNIFICANCE
PUPATION CHAMBERS
SPHINX MOTH
TEISSEIREI BARATTINIA
title_short Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall
title_full Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall
title_fullStr Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall
title_full_unstemmed Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall
title_sort Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall
dc.creator.none.fl_str_mv Genise, Jorge Fernando
Farina, Juan Luis
Verde, Mariano
author Genise, Jorge Fernando
author_facet Genise, Jorge Fernando
Farina, Juan Luis
Verde, Mariano
author_role author
author2 Farina, Juan Luis
Verde, Mariano
author2_role author
author
dc.subject.none.fl_str_mv MULTI-LAYERED WALL
PALAEOPEDOLOGICAL SIGNIFICANCE
PUPATION CHAMBERS
SPHINX MOTH
TEISSEIREI BARATTINIA
topic MULTI-LAYERED WALL
PALAEOPEDOLOGICAL SIGNIFICANCE
PUPATION CHAMBERS
SPHINX MOTH
TEISSEIREI BARATTINIA
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The trace fossil Teisseirei barattinia, found in Cenozoic formations of Uruguay and Argentina, is an elongated chamber recognizable by its depressed cross-section, antechamber, and its multi-layered lining with an inner surface texture composed of densely packed sub-rectangular to sub-triangular pits. Our recent behavioural observations on larval and pupal stages of Sphingidae (Lepidoptera), particularly on Manduca rustica, suggest that Teisseirei barattinia is the pupation chamber of a sphinx moth. Last instar larvae of Manduca rustica, Eumorpha anchemolus and E. labruscae were placed in terraria to observe their burrowing behaviour and to recover pupation chambers. Chambers show depressed or plane convex cross-sections as T. barattinia. The internal surface texture of walls is also similar to that of T. barattinia. The same pattern could be obtained experimentally by pressing the true legs of Manduca rustica larva against plasticine. The multi-layered wall structure, shown by T. barattinia, is a new type of lining for insect trace fossils in palaeosols that result from soil packing combined with discharges of abundant liquid excretion by soft-bodied larvae, as in the case of Manduca rustica. T. barattinia is the first trace fossil documented in palaeosols attributed to sphinx moths and supported by macro and micromorphological comparisons with extant pupation chambers. The shallow emplacement of moth pupation chambers in soils suggests that T. barattinia would be a good indicator of palaeosol upper horizons.
Fil: Genise, Jorge Fernando. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales; Argentina. Universidad de la Republica. Facultad de Ciencias;
Fil: Farina, Juan Luis. Provincia de Buenos Aires. Municipalidad de General Pueyrredon. Secretaria de Cultura. Museo Municipal de Cs Naturales Lorenzo Scaglia; Argentina
Fil: Verde, Mariano. Universidad de la República; Uruguay
description The trace fossil Teisseirei barattinia, found in Cenozoic formations of Uruguay and Argentina, is an elongated chamber recognizable by its depressed cross-section, antechamber, and its multi-layered lining with an inner surface texture composed of densely packed sub-rectangular to sub-triangular pits. Our recent behavioural observations on larval and pupal stages of Sphingidae (Lepidoptera), particularly on Manduca rustica, suggest that Teisseirei barattinia is the pupation chamber of a sphinx moth. Last instar larvae of Manduca rustica, Eumorpha anchemolus and E. labruscae were placed in terraria to observe their burrowing behaviour and to recover pupation chambers. Chambers show depressed or plane convex cross-sections as T. barattinia. The internal surface texture of walls is also similar to that of T. barattinia. The same pattern could be obtained experimentally by pressing the true legs of Manduca rustica larva against plasticine. The multi-layered wall structure, shown by T. barattinia, is a new type of lining for insect trace fossils in palaeosols that result from soil packing combined with discharges of abundant liquid excretion by soft-bodied larvae, as in the case of Manduca rustica. T. barattinia is the first trace fossil documented in palaeosols attributed to sphinx moths and supported by macro and micromorphological comparisons with extant pupation chambers. The shallow emplacement of moth pupation chambers in soils suggests that T. barattinia would be a good indicator of palaeosol upper horizons.
publishDate 2013
dc.date.none.fl_str_mv 2013-07
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/1364
Genise, Jorge Fernando; Farina, Juan Luis; Verde, Mariano; Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall; Wiley Blackwell Publishing, Inc; Lethaia; 46; 4; 7-2013; 480-489
0024-1164
url http://hdl.handle.net/11336/1364
identifier_str_mv Genise, Jorge Fernando; Farina, Juan Luis; Verde, Mariano; Teisseirei barattinia Roselli 1939: the first sphinx moth trace fossil from palaeosols and its distinct type of wall; Wiley Blackwell Publishing, Inc; Lethaia; 46; 4; 7-2013; 480-489
0024-1164
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1111/let.12025
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Wiley Blackwell Publishing, Inc
publisher.none.fl_str_mv Wiley Blackwell Publishing, Inc
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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