scholarly journals The early wasp plucks the flower: disparate extant diversity of sawfly superfamilies (Hymenoptera: ‘Symphyta’) may reflect asynchronous switching to angiosperm hosts

2019 ◽  
Vol 128 (1) ◽  
pp. 1-19
Author(s):  
Tommi Nyman ◽  
Renske E Onstein ◽  
Daniele Silvestro ◽  
Saskia Wutke ◽  
Andreas Taeger ◽  
...  
Keyword(s):  
Mass Extinction ◽  
Insect Herbivore ◽  
Ancestral State ◽  
Asynchronous Switching ◽  
Time Intervals ◽  
Diversification Rates ◽  
Insect Order ◽  
Plant Associations ◽  
Diversity Dynamics ◽  
Herbivore Communities

AbstractThe insect order Hymenoptera originated during the Permian nearly 300 Mya. Ancestrally herbivorous hymenopteran lineages today make up the paraphyletic suborder ‘Symphyta’, which encompasses c. 8200 species with very diverse host-plant associations. We use phylogeny-based statistical analyses to explore the drivers of diversity dynamics within the ‘Symphyta’, with a particular focus on the hypothesis that diversification of herbivorous insects has been driven by the explosive radiation of angiosperms during and after the Cretaceous. Our ancestral-state estimates reveal that the first symphytans fed on gymnosperms, and that shifts onto angiosperms and pteridophytes – and back – have occurred at different time intervals in different groups. Trait-dependent analyses indicate that average net diversification rates do not differ between symphytan lineages feeding on angiosperms, gymnosperms or pteridophytes, but trait-independent models show that the highest diversification rates are found in a few angiosperm-feeding lineages that may have been favoured by the radiations of their host taxa during the Cenozoic. Intriguingly, lineages-through-time plots show signs of an early Cretaceous mass extinction, with a recovery starting first in angiosperm-associated clades. Hence, the oft-invoked assumption of herbivore diversification driven by the rise of flowering plants may overlook a Cretaceous global turnover in insect herbivore communities during the rapid displacement of gymnosperm- and pteridophyte-dominated floras by angiosperms.

scholarly journals Plant and insect herbivore community variation across the Paleocene–Eocene boundary in the Hanna Basin, southeastern Wyoming

PeerJ ◽  
2019 ◽  
Vol 7 ◽  
pp. e7798
Author(s):  
Lauren E. Azevedo Schmidt ◽  
Regan E. Dunn ◽  
Jason Mercer ◽  
Marieke Dechesne ◽  
Ellen D. Currano
Keyword(s):  
Community Composition ◽  
Plant Communities ◽  
Plant Diversity ◽  
High Water ◽  
Insect Herbivore ◽  
Herbivore Damage ◽  
Late Paleocene ◽  
Hanna Basin ◽  
Laramide Basins ◽  
Herbivore Communities

Ecosystem function and stability are highly affected by internal and external stressors. Utilizing paleobotanical data gives insight into the evolutionary processes an ecosystem undergoes across long periods of time, allowing for a more complete understanding of how plant and insect herbivore communities are affected by ecosystem imbalance. To study how plant and insect herbivore communities change during times of disturbance, we quantified community turnover across the Paleocene­–Eocene boundary in the Hanna Basin, southeastern Wyoming. This particular location is unlike other nearby Laramide basins because it has an abundance of late Paleocene and Eocene coal and carbonaceous shales and paucity of well-developed paleosols, suggesting perpetually high water availability. We sampled approximately 800 semi-intact dicot leaves from five stratigraphic levels, one of which occurs late in the Paleocene–Eocene thermal maximum (PETM). Field collections were supplemented with specimens at the Denver Museum of Nature & Science. Fossil leaves were classified into morphospecies and herbivore damage was documented for each leaf. We tested for changes in plant and insect herbivore damage diversity using rarefaction and community composition using non-metric multidimensional scaling ordinations. We also documented changes in depositional environment at each stratigraphic level to better contextualize the environment of the basin. Plant diversity was highest during the mid-late Paleocene and decreased into the Eocene, whereas damage diversity was highest at the sites with low plant diversity. Plant communities significantly changed during the late PETM and do not return to pre-PETM composition. Insect herbivore communities also changed during the PETM, but, unlike plant communities, rebound to their pre-PETM structure. These results suggest that insect herbivore communities responded more strongly to plant community composition than to the diversity of species present.

scholarly journals Long‐term restoration success of insect herbivore communities in seminatural grasslands: a functional approach

2020 ◽  
Vol 30 (6) ◽  
Author(s):  
Felix Neff ◽  
M. Carol Resch ◽  
Anja Marty ◽  
Jacob D. Rolley ◽  
Martin Schütz ◽  
...  
Keyword(s):  
Functional Approach ◽  
Insect Herbivore ◽  
Restoration Success ◽  
Seminatural Grasslands ◽  
Herbivore Communities

The Influence of Soil Type on Rain Forest Insect Herbivore Communities

Biotropica ◽  
2008 ◽  
Vol 40 (6) ◽  
pp. 707-713 ◽  
Author(s):  
Markus P. Eichhorn ◽  
Stephen G. Compton ◽  
Sue E. Hartley
Keyword(s):  
Soil Type ◽  
Rain Forest ◽  
Insect Herbivore ◽  
Forest Insect ◽  
Herbivore Communities

scholarly journals Seed plant families with diverse mycorrhizal states have higher diversification rates

2019 ◽  
Author(s):  
María Isabel Mujica ◽  
Gustavo Burin ◽  
María Fernanda Pérez ◽  
Tiago Quental
Keyword(s):  
Soil Fungi ◽  
Plant Evolution ◽  
Ancestral State ◽  
Seed Plant ◽  
Plant Family ◽  
Symbiotic Interaction ◽  
Evolutionary Transitions ◽  
Diversification Rates ◽  
Plant Families ◽  
The Relationship

AbstractA crucial innovation in plant evolution was the association with soil fungi during land colonization. Today, this symbiotic interaction is present in most plants species and can be classified in four types: arbuscular (AM), Ecto (EM), Orchid (OM) and Ericoid Mycorrhiza (ER). Since the AM ancestral state, some plants lineages have switched partner (EM, OM and ER) or lost the association (no-association: NM). Evolutionary transitions to a novel mycorrhizal state (MS) might allow plant lineages to access new resources, enhancing diversification rates. However, some clades are not restricted to one MS, and this variability might promote diversification. In this study we address the relationship between MS and diversification rates of seed plant families. For this, we used the recently published FungalRoot database, which compiled data for 14,870 species and their mycorrhizal partners. We assigned a MS to each plant family, calculated the MS heterogeneity and estimated their diversification rates using the method-of-moments. Families with mixed MS had the highest diversification rates and there was a positive relationship between MS heterogeneity and diversification rates. These results support the hypothesis that MS lability promotes diversification and highlight the importance of the association with soil fungi for the diversification of plants.

INSECT HERBIVORE COMMUNITIES TRACKED THE CONIFER AGATHIS (ARAUCARIACEAE) FROM PALEOGENE PATAGONIA TO MODERN AUSTRALASIA AND SOUTHEAST ASIA

2016 ◽  
Author(s):  
Michael P. Donovan ◽  
◽  
Conrad C. Labandeira ◽  
Conrad C. Labandeira ◽  
Ari Iglesias ◽  
...  
Keyword(s):  
Southeast Asia ◽  
Insect Herbivore ◽  
Herbivore Communities

Permian–Triassic land-plant diversity in South China: Was there a mass extinction at the Permian/Triassic boundary?

Paleobiology ◽  
2011 ◽  
Vol 37 (1) ◽  
pp. 157-167 ◽  
Author(s):  
Conghui Xiong ◽  
Qi Wang
Keyword(s):  
South China ◽  
Mass Extinction ◽  
Middle Triassic ◽  
Land Plant ◽  
Land Plants ◽  
Late Triassic ◽  
Triassic Boundary ◽  
Permian Triassic Boundary ◽  
Diversity Dynamics ◽  
Early Middle Triassic

Diversity dynamics of the Permian–Triassic land plants in South China are studied by analyzing paleobotanical data. Our results indicate that the total diversity of land-plant megafossil genera and species across the Permian/Triassic boundary (PTB) of South China underwent a progressive decline from the early Late Permian (Wuchiapingian) to the Early-Middle Triassic. In contrast, the diversity of land-plant microfossil genera exhibited only a small fluctuation across the PTB of South China, showing an increase at the PTB. Overall, land plants across the PTB of South China show a greater stability in diversity dynamics than marine faunas. The highest extinction rate (90.91%) and the lowest origination rate (18.18%) of land-plant megafossil genera occurred at the early Early Triassic (Induan), but the temporal duration of the higher genus extinction rates (>60%) in land plants was about 23.4 Myr, from the Wuchiapingian to the early Middle Triassic (Anisian), which is longer than that of the coeval marine faunas (3–11 Myr). Moreover, the change of genus turnover rates in land-plant megafossils steadily fluctuated from the late Early Permian to the Late Triassic. More stable diversity and turnover rate as well as longer extinction duration suggest that land plants near the PTB of South China may have been involved in a gradual floral reorganization and evolutionary replacement rather than a mass extinction like those in the coeval marine faunas.

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