Review Article |
Corresponding author: David J. Wildish ( talitridnb@gmail.com ) Academic editor: Pedro Taucce
© 2023 David J. Wildish, John H. McDonald.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
Wildish DJ, McDonald JH (2023) Possible causes of amphi-Atlantic distribution of Orchestia gammarellus (Pallas, 1776) (Crustacea, Amphipoda, Talitridae) in the North Atlantic: a review. Zoosystematics and Evolution 99(1): 55-62. https://doi.org/10.3897/zse.99.95980
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Hypotheses concerning the modern distribution of Orchestia gammarellus (Crustacea, Amphipoda, Talitridae) and its causes in the North Atlantic are discussed. The synanthropic dispersal hypothesis of
evolution, dispersal, North Atlantic, O. gammarellus, zoogeography
The talitrid amphipod Orchestia gammarellus (Pallas, 1766) occurs in the supralittoral of both north-eastern and north-western coasts of the Atlantic Ocean. It is one of only three North Atlantic talitrids, the other two being Platorchestia platensis (Krøyer, 1845) and P. monodi (Mateus, Mateus & Alfonso, 1986), which are amphi-Atlantic (
In this presentation, the literature on O. gammarellus is reviewed as it pertains to its distribution and origins on both coasts of the North Atlantic Ocean.
The known distribution of O. gammarellus within the North Atlantic Ocean is shown in Fig.
Map of the North Atlantic showing the distribution of O. gammarellus. Dashed line indicates intermittent presence on Canadian shores. Continuous line indicates presence (but not necessarily contiguous distribution) on Icelandic, European and Atlantic archipelago shores. Fill lines suggests presence at some coastal locations within each inland Sea. Question marks indicate that no published data of O. gammarellus distribution were found in this area.
We note that only one species of true Orchestia Leach, 1814: O. gammarellus (= O. forchuensis Myers & Lowry, 2020) is present on the northwest Atlantic coast. On the north-eastern Atlantic/Mediterranean coasts, there are at least five species present: O. gammarellus, O. mediterranea A Costa, 1857, O. aestuarensis Wildish, 1987, O. montagui (Audouin, 1826) and O. xylino Lowry & Fanini, 2013. However, two independent molecular phylogenies (
In summary, O. gammarellus is present on the eastern shore of the North Atlantic Ocean between the geographical bounds of 28 to 68°N, and on the western shore between 44 and 65°N.
Three hypotheses concerning the evolution of O. gammarellus in the North Atlantic Ocean have been proposed:
A morphological analysis of 16 O. gammarellus populations from Canadian, Icelandic and European locations was conducted by
These characters apply to adults and cannot distinguish immatures and juvenile members of the two populations.
Morphological plasticity has been recognised within talitrids, notably those species living in a wrack primary ecotope, such as Platorchestia platensis. Platorchestia platensis can acclimate to a secondary ecotope: driftwood (
Apart from the three amphi-Atlantic talitrids, inclusive of O. gammarellus, the talitrid biodiversity of the east and west coasts of the North Atlantic Ocean lack species in common (table 1 in
Apart from the three amphi-Atlantic species, the different talitrid fauna on both coasts we consider as evidence that long-term separation occurred after isolation of the two coasts by continental drift in the upper Cretacious/Eocene (
In post-glacial times, colonising O. gammarellus in Iceland would reach an open supralittoral wrack habitat, without competitors, whereas in Newfoundland and Maritime Canada, they would compete with P. platensis, which was spreading northwards following glacial retreat. Competition between these two species (
Sceptics of dispersal have condemned it as immeasurable and unimportant, but evidence of a resurgence of interest in natural dispersal was identified by
The range of O. gammarellus, from the north-eastern Atlantic Islands (Azores, Madeira, Canaries) to the Lofoten Islands, demonstrates that this species has dispersed widely within the North Atlantic. In a largely theoretical study of dispersal,
Within the last ten thousand years, during which humans have travelled to most parts of the planet and established trading routes by marine transport, they have often taken with them hitchhikers which colonise the new habitats. This process of synanthropy has been identified amongst talitrids, particularly those of terrestrial origin which come in soil or attached to imported tropical plants (e.g.
The alternative mechanism of natural dispersal considered by
Genetically separate lineages of multicellular organisms accumulate increasing amounts of DNA sequences which diverge during the passage of time. As a result, it is possible to estimate the geological time at which divergence first occurred using DNA sequence data. The mitochondrial cytochrome oxidase I (COI) gene is widely used for species identification and can also be used to estimate divergence times of two genetically separate lineages.
Other published molecular data of pairs of closely related species generally differ in their COI sequences by several percent;
We used MEGA version 11 (
Molecular genetic methods applied to amphipod taxonomy are an important addition to morphology, rather than a replacement of it, resulting in a more accurate and useful combined discipline. The particular molecular genetic methods needed to achieve this include:
The COI phylogeny of
Since the dispersal and zoogeographic distribution of Orchestia in the North Atlantic is hypothesised to occur either in the recent post-glacial or distant (Eocene/Cretaceous) past, direct evidence to determine how it happened is impossible to obtain. Consequently, the best approach to this question is to use an accumulation of indirect, circumstantial evidence inclusive of molecular genetic methods, to determine which hypothesis is more likely to be the correct one. The circumstantial evidence, so far available, favours post-glacial natural dispersal. In summary the arguments for this point of view are as follows:
Given that post-glacial natural dispersal of O. gammarellus in the North Atlantic is the more plausible one, we question the validity of a new species name: O. forchuensis Myers & Lowry, 2020, proposed for the Canadian/Icelandic specimens. Paraphrasing
We thank Dr. Christine Henzler of the Minnesota Supercomputing Institute, University of Minnesota, U. S. A. and Dr. Jorge Pérez-Schultheiss, Museo Nacional de Historia Natural, Chile for comments and improvements to the manuscript.