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Haemaphysalis cretacea a nymph of a new species of hard tick in Burmese amber

Published online by Cambridge University Press:  12 April 2018

Lidia Chitimia-Dobler
Affiliation:
Bundeswehr Institute of Microbiology, Neuherbergstrasse 11, D-80937 Munich, Germany German Center of Infection Research (DZIF) Partner Munich
Timo Pfeffer
Affiliation:
Keyence Deutschland GmbH, Siemensstrasse 1, 63263 Neu-Isenburg, Germany
Jason A Dunlop*
Affiliation:
Museum für Naturkunde, Leibniz Institute for Evolution and Biodiversity Science, Invalidenstrasse 43, D-10115 Berlin, Germany
*
Author for correspondence: Jason A Dunlop, E-mail: jason.dunlop@mfn-berlin.de

Abstract

The first fossil potentially assignable to the extant hard tick genus Haemaphysalis CL Koch (1844) (Ixodida: Ixodidae) is described from the Late Cretaceous (ca. 99 Ma) Burmese amber of Myanmar. Haemaphysalis (Alloceraea) cretacea sp. nov. is the oldest and only fossil representative of this genus; living members of which predominantly feed on mammals. Their typical hosts are known since at least the Jurassic and the discovery of a mid-Cretaceous parasite, which might have fed on mammals raises again the question of to what extent ticks are coupled to their (modern) host groups. An inferred Triassic split of Argasidae (soft ticks) into the bird-preferring Argasinae and mammal-preferring Ornithodorinae dates to about the time when dinosaurs (later including birds) and mammaliaforms as potential hosts were emerging. Ixodidae may have split into Prostriata and Metastriata shortly after the end-Permian mass extinction, an event which fundamentally altered the terrestrial vertebrate fauna. Prostriata (the genus Ixodes) prefer birds and mammals today, and some may have used groups like cynodonts in the Triassic. Basal metastriate ticks (e.g. Amblyomma) prefer reptiles, but derived metastriates (including Haemaphysalis) again prefer mammals. Here, we may be looking at a younger (Cretaceous?) shift associated with more recent mammalian radiations.

Type
Research Article
Copyright
Copyright © Cambridge University Press 2018 

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