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ORIGINAL RESEARCH article

Front. Ecol. Evol.
Sec. Paleoecology
Volume 12 - 2024 | doi: 10.3389/fevo.2024.1381539
This article is part of the Research Topic Changes in Plant-Herbivore Interactions Across Time Scales: Bridging Paleoecology and Contemporary Ecology View all 4 articles

Plant-insect interactions in the mid-Cretaceous paleotropical El Chango Lagerstätte (Cintalapa Fm., Mexico)-patterns of herbivory during the Angiosperm Terrestrial Revolution

Provisionally accepted
Artai A. Santos Artai A. Santos 1*Stephen McLoughlin Stephen McLoughlin 1,2Marco A. Rubalcaba-Knoth Marco A. Rubalcaba-Knoth 2*Ana L. Hernández-Damian Ana L. Hernández-Damian 2*Uxue Villanueva-Amadoz Uxue Villanueva-Amadoz 2*Sergio R. Cevallos-Ferriz Sergio R. Cevallos-Ferriz 2*
  • 1 Swedish Museum of Natural History, Stockholm, Sweden
  • 2 Instituto de Geología, UNAM,, México D. F., Mexico

The final, formatted version of the article will be published soon.

    Plants and insects are two of the more diverse and abundant organisms in terrestrial ecosystems. The fossil record of plant-insect interactions offers crucial insights into the coevolutionary dynamics between these groups, shedding light on the intricate relationships that have shaped terrestrial ecosystems. The study of fossil interactions is especially relevant in mid-Cretaceous ecosystems, a time of dramatic changes in the composition of floras and, consequently, in plant-insect relationships. Here, we describe the first suite of plant-insect interactions from the mid-Cretaceous of Mexico. We studied 554 plant fossils from the El Chango Lagerstätte (Cintalapa Formation, Chiapas, Mexico), including vegetative (leaves) and reproductive structures (fruits and seeds). The flora was dominated by gymnosperms (89.3%) followed by angiosperms (10.7%); other groups, such as pteridophytes and bryophytes, were absent. In total, 5.4% of the plant specimens hosted some damage. Angiosperms (all broad-leafed forms), despite being much less common than gymnosperms, expressed more evidence of damage by herbivores (35.6% of specimens damaged). In contrast, the narrow-leafed gymnosperms, the dominant group in the flora, hosted a much lower proportion of herbivory damage (1.8% of specimens damaged). The diversity of damage types (DTs) was relatively low: 14 DTs were identified, corresponding to seven FFGs, including margin feeding, hole feeding, surface feeding, piercing and sucking, oviposition, galling, and mining. Comparison with the other mid-Cretaceous plant-insect assemblages reveals a similar richness of DTs for angiosperms but a lower richness and diversity of DTs on gymnosperms from El Chango.These results indicate preferential herbivory on angiosperms (rather than on the available gymnosperms in the assemblage) by terrestrial arthropods during a period of major changes in the structure of terrestrial ecosystems. However, it is challenging to resolve whether this apparent preference is because insects particularly targeted angiosperms or if the herbivores simply targeted broad leaves in general, since all the available gymnosperms from El Chango are scale-leafed forms.

    Keywords: Angiosperms, Gymnosperms, Mid-Cretaceous, plant-arthropod interactions, Palaeoecology, Fruits, Herbivory

    Received: 03 Feb 2024; Accepted: 17 Jun 2024.

    Copyright: © 2024 Santos, McLoughlin, Rubalcaba-Knoth, Hernández-Damian, Villanueva-Amadoz and Cevallos-Ferriz. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

    * Correspondence:
    Artai A. Santos, Swedish Museum of Natural History, Stockholm, Sweden
    Marco A. Rubalcaba-Knoth, Instituto de Geología, UNAM,, México D. F., Mexico
    Ana L. Hernández-Damian, Instituto de Geología, UNAM,, México D. F., Mexico
    Uxue Villanueva-Amadoz, Instituto de Geología, UNAM,, México D. F., Mexico
    Sergio R. Cevallos-Ferriz, Instituto de Geología, UNAM,, México D. F., Mexico

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