PLANT-INSECT INTERACTIONS ON DICOTS AND FERNS FROM THE MIOCENE OF ARGENTINA
2018; Society for Sedimentary Geology; Volume: 33; Issue: 7 Linguagem: Inglês
10.2110/palo.2017.100
ISSN1938-5323
AutoresJuan M. Robledo, Esther R. S. Pinheiro, Silvia Gnaedinger, Torsten Wappler,
Tópico(s)Ecology and Vegetation Dynamics Studies
ResumoResearch Article| July 24, 2018 PLANT-INSECT INTERACTIONS ON DICOTS AND FERNS FROM THE MIOCENE OF ARGENTINA JUAN M. ROBLEDO; JUAN M. ROBLEDO 1Centro de Ecología Aplicada del Litoral (CECOAL), CONICET, Ruta 5, km 2,5, Casilla correo 291, 3400, Corrientes, Argentina Search for other works by this author on: GSW Google Scholar ESTHER R. S. PINHEIRO; ESTHER R. S. PINHEIRO 2Geological Museum, University of Wyoming, 1000E University Avenue, 82072, Laramie, Wyoming, USA Search for other works by this author on: GSW Google Scholar SILVIA C. GNAEDINGER; SILVIA C. GNAEDINGER 1Centro de Ecología Aplicada del Litoral (CECOAL), CONICET, Ruta 5, km 2,5, Casilla correo 291, 3400, Corrientes, Argentina 3Facultad de Ciencias Exactas y Naturales y Agrimensura, Universidad Nacional del Nordeste (FaCENA-UNNE), Ruta 5, Km 2,5, Casilla correo 291, 3400, Corrientes, Argentina Search for other works by this author on: GSW Google Scholar TORSTEN WAPPLER TORSTEN WAPPLER 4Hessisches Landesmuseum Darmstadt, Darmstadt, Germany Search for other works by this author on: GSW Google Scholar Author and Article Information JUAN M. ROBLEDO 1Centro de Ecología Aplicada del Litoral (CECOAL), CONICET, Ruta 5, km 2,5, Casilla correo 291, 3400, Corrientes, Argentina ESTHER R. S. PINHEIRO 2Geological Museum, University of Wyoming, 1000E University Avenue, 82072, Laramie, Wyoming, USA SILVIA C. GNAEDINGER 1Centro de Ecología Aplicada del Litoral (CECOAL), CONICET, Ruta 5, km 2,5, Casilla correo 291, 3400, Corrientes, Argentina 3Facultad de Ciencias Exactas y Naturales y Agrimensura, Universidad Nacional del Nordeste (FaCENA-UNNE), Ruta 5, Km 2,5, Casilla correo 291, 3400, Corrientes, Argentina TORSTEN WAPPLER 4Hessisches Landesmuseum Darmstadt, Darmstadt, Germany e-mail: manuelrobledo@conicet.gov.ar Publisher: SEPM Society for Sedimentary Geology First Online: 24 Jul 2018 Online Issn: 1938-5323 Print Issn: 0883-1351 Copyright © 2018, SEPM (Society for Sedimentary Geology) PALAIOS (2018) 33 (7): 338–352. https://doi.org/10.2110/palo.2017.100 Article history First Online: 24 Jul 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation JUAN M. ROBLEDO, ESTHER R. S. PINHEIRO, SILVIA C. GNAEDINGER, TORSTEN WAPPLER; PLANT-INSECT INTERACTIONS ON DICOTS AND FERNS FROM THE MIOCENE OF ARGENTINA. PALAIOS 2018;; 33 (7): 338–352. doi: https://doi.org/10.2110/palo.2017.100 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 The study of plant-insect interactions provides valuable information about the ecology of feeding behavior and the relationships between the host plant and the producer insect. Records of feeding traces are relatively rare for the Miocene of South America. Here, new records of plant-insect interactions on dicot leaves and fern fronds from the middle and late Miocene of Argentina are presented. In total, 1204 dicot and fern impressions were analyzed including 384 from the San José Formation and 856 from the Palo Pintado Formation. Traces of arthropod herbivory are found on 303 foliar impressions, 288 from the Palo Pintado Formation and just 15 from the San José Formation. Forty-four percent of all traces were found on Thelypteris interrupta (Willd.) Iwatsuki 1963 (Thelypteridaceae), followed by Cedrela fissiliformisAnzótegui and Horn 2011 (Meliaceae) (15.1%) and Schinus herbstiiAnzótegui 1998 (Anacardiaceae) (11.3%). Thelypteris interrupta is associated with a low diversity of Damage Types, mainly hole and window feedings, indicating a monospecific relationship with the trace maker. On the other hand, the high abundance and diversity of damage types found on C. fissiliformis and S. herbstii denote that these plants were hosting a more diverse group of arthropods. Likewise, the lower number of traces identified in the San José Formation corresponds to the xeric conditions established during the middle Miocene in northwestern Argentina. These conditions changed in the late Miocene, at least in some regions, to a humid climate, promoting an increase in phytophagy that is evidenced by the abundance recorded in the Palo Pintado Formation. 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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