1. Introduction
The relationships among species diversity, latitude, and altitude are of fundamental interest to ecologists and biogeographers and are expected to undergo significant changes, both globally and in New Zealand, as a result of climate change [
1,
2]. Species diversity is commonly greater at lower than higher latitudes on a global scale, and the similarity of communities commonly decreases with distance [
3,
4]. Although the reasons for this common global pattern are not well understood [
5], Fine [
6] noted that tropical regions are the source of almost all groups of organisms and, in contrast to lands at higher latitudes, their greater extent and climatic stability during the last 10–50 million years have promoted increased speciation and reduced extinction rates. The geographical distribution of stream-dwelling insects was reviewed by Vinson and Hawkins [
7], who found that patterns of distribution in relation to latitude differed among insect groups and that the generic richness of Ephemeroptera (mayflies) and Plecoptera (stoneflies) tended to be higher in temperate than tropical regions. Similarly, Pearson and Boyero [
8] showed that species richness in these two insect orders tended to be higher at higher latitudes, although considerable variation was found on latitudinal gradients. Some of this variation is undoubtedly due to historical factors, including past speciation and extinction, as well as spatial and environmental processes [
9]. Thus, community assembly (species sorting) can be mediated by the abiotic conditions and inter-species competition in the local environment, by regional factors that influence dispersal, and immigration to a local community [
10,
11], as well as by present and former land-use [
12]. For example, in an extensive study of Brazilian streams, the community composition of Ephemeroptera was more strongly influenced by environmental (physico-chemical) factors than spatial processes [
13].
It is also common for species richness of aquatic fauna to decline with increasing altitude, and the assemblage composition of stream invertebrates can also change profoundly, as found in the Himalayas of Nepal [
14,
15]. Although the factors determining altitudinal patterns are poorly known [
16], temperature was clearly the best predictor of species richness for both plants and animals along a 3.7 km elevational gradient on Mount Kilimanjaro, Africa [
17]. Ward [
18] also implicated temperature as a prime determinant of the distribution, diversity, and abundance of aquatic insects along altitudinal gradients, a role that is hardly surprising given that it is a key factor affecting their growth, metabolism, reproduction, and emergence [
19].
New Zealand is well suited for undertaking a latitudinal study as it is a narrow country whose three main islands extend over almost 13 degrees of latitude and whose mean air temperature declines by about 6 °C from north to south [
20]. The country also possesses substantial mountain ranges and reasonable road access to about 1000 m a. s. l., which is close to the upper tree line, enabling altitudinal studies. A mean annual decline in temperature of −0.5 °C per 100 m has been reported from New Zealand [
20], although the rate can be expected to vary depending on local topography and meteorological conditions [
21].
The New Zealand mayfly fauna comprises 59 described species in 20 endemic genera and eight families, three of which are also endemic to the country [
22,
23,
24]. The fauna shows close relationships with the mayflies of southern South America and Australia [
25,
26], which, like New Zealand, were parts of the ancient continent of Gondwana [
27]. A number of the extant leptophlebiid genera also show affinities with New Caledonia [
28], which, along with New Zealand, is an exposed fragment of the submerged Gondwanan landmass of Zealandia [
29]. The distributions of New Zealand mayfly species have not been investigated systematically, but museum collections and general collecting, primarily for taxonomic purposes, suggest that more species are present in the northern and lowland streams than in the south of the country and at higher altitudes [
28,
30].
The aim of our study was to investigate the latitudinal and altitudinal distributions of New Zealand mayfly communities by means of an extensive and systematic nationwide survey incorporating light-trapping of imagos and subimagos and the collection of nymphs from streams. A subsidiary study was also undertaken at seven sites on Mount Taranaki, a prominent inactive volcano in the east of North Island, in which the confounding effect of latitude was factored out. We tested the hypothesis that species richness of mayflies in natural (unimpacted), predominantly forested, New Zealand streams would decline with increasing latitude and altitude, and that species turnover (beta diversity) would occur along both the latitudinal and elevational gradients in parallel with changes in species richness.
4. Discussion
We found that the species richness of the mayflies declined significantly from the north to the south in New Zealand, despite the gradient extending over only 13 degrees of latitude. A comparable relationship between latitude and species richness was also reported for Australia by Lake et al. [
49], who sampled stones in geomorphologically similar streams using a standardized procedure and found more invertebrate species in the tropical than the temperate regions of the country. Nevertheless, the diversity of higher aquatic taxa, such as insect orders, can differ greatly among streams along tropical–temperate gradients in Australia and elsewhere because of their great range of physico-chemical, hydrological, and climatic conditions, characteristics that inevitably confound regional patterns of taxonomic richness [
50].
The relationship we found between species richness and altitude in our nationwide dataset was weaker than that between richness and latitude. The number of mayfly species in forest streams of comparable size, physico-chemistry, and surrounding vegetation also declined noticeably at sites > 730 m a. s. l. on Mount Taranaki and therefore showed a comparable pattern to that which was found in the nationwide survey. Together, these results are consistent with those of studies elsewhere, which indicate that species richness of Ephemeroptera is negatively associated with altitude and that altitude-related variables such as temperature play important roles in structuring mayfly communities [
51,
52].
In addition to a decline in species richness, the turnover (beta diversity) of mayfly communities increased from north to south, reflecting differences in the latitudinal distributions of individual species. Thus, of the 53 species recorded, only 11 were widespread across both North and South Islands, but 17 were found only on North Island and 16 only on South Island. Furthermore, some species were confined to the northernmost zones of the country, while others occurred throughout North Island, and a suite of species were found only in two or three South Island zones. A pattern of steadily declining species richness from north to south within New Zealand has also been described for canopy trees [
53], although in the far north, where mayfly diversity is high, species richness of trees was low. McGlone et al. [
53] postulated that the small land area of the Northland–Auckland peninsula was the reason for the low tree diversity there. In contrast, the northernmost region of the country has very high numbers of regionally endemic insect taxa, terrestrial amphipods, and land snails [
54,
55,
56], and the exceptional richness of mayfly species in Northland may reflect its historical role as a faunal refuge and site of evolution during the Pleistocene ice ages [
57,
58,
59]. Subsequent dispersal from this refuge is perceived to have extended the distributions of mayfly species southward to various extents, but Cook Strait and its predecessor, the Manawatu Strait [
60], may have acted as barriers to the dispersal of mayflies into South Island [
61]. Hence, the latitudinal pattern of change in species distributions from the north to the south can be explained, at least in part.
Deleatidium, however, with 21 described species, 10 of which are restricted to the South Island, appears to be an important exception to the above scenario. Thus, Hitchings [
61,
62] postulated that the formation of the Southern Alps and other South Island mountain ranges in the Miocene–Pliocene, and periodic advances and retreats of glaciers in the Pleistocene, would have resulted in the formation and diversification of new habitat and may have favored the speciation of
Deleatidium. A similar scenario has been proposed for New Zealand blackflies (Diptera: Simuliidae) [
63] and stoneflies (Plecoptera) [
64], aquatic insects that are more strongly represented in the South Island and do not show a decline in species richness from the north to the south [
63,
65]. Today, nymphs of many
Deleatidium species are found in moderate to fast-flowing waters, including many unstable, physically disturbed streams and rivers that characterize the South Island mountains [
66]. In contrast, the nymphs of mayflies in several other genera of Leptophlebiidae found predominantly in the north tend to occur in slow-flowing parts of forest streams at low altitudes, consistent with a northern evolutionary origin in a less-mountainous environment [
28].
As is well known, local environmental factors and the availability of a suitable habitat have important roles in structuring running water communities [
67]. A pertinent example is the extensive Brazilian study of Shimano et al. [
13], which indicated that environmental factors, including stream width, had a more significant role than spatial factors in structuring mayfly communities. Similarly, recent studies of New Zealand macroinvertebrate communities inhabiting riffles in forest streams suggested that habitat diversity had stronger effects on invertebrate richness than regional- or landscape-level factors [
11,
45]. While we did not explicitly investigate the role of local environmental and habitat factors on the distribution of mayflies, significant relationships with temperature, stream width, canopy cover, and conductivity suggest they are contributing factors in addition to latitude in determining ephemeropteran community composition and richness in New Zealand. Our results also suggest that the declining gradient in species richness from the north to the south probably has historical origins, with the north of the country having acted as a major refuge and region of speciation during the Pleistocene. The increasing dissimilarity of the northern and southern mayfly communities not only reflects differences in subsequent southward dispersal of these species but the presence of South Island species, which evolved in its mountains.
Because of its focus on latitude and altitude, our study has the potential to provide a basis for assessing the effects of ongoing climate change on New Zealand’s stream-dwelling Ephemeroptera and for evaluating their conservation needs. Over the course of the last century, there has been an increased frequency of extreme weather events, including warmer annual temperatures and reduced alpine snowfall [
68,
69]. These changes and the retreat and loss of glaciers have altered stream flows and habitats and can be expected to continue to affect the distribution of mayflies and other stream fauna, especially in the mountains. With an increase in temperature, the distributions of some species may move to higher altitudes or into cooler waters further south, but inhabitants of extreme cold-water habitats below the faces of glaciers are likely to be vulnerable to extinction [
2,
70].
In our nationwide survey, we recorded range-restricted mayfly species in many parts of the country, including the South Island mountains where several alpine and sub-alpine species of
Deleatidium are potentially at risk [
62,
70]. Similarly, on Mount Taranaki,
D. magnum and
Oniscigaster distans were only found at the highest sites. Although
D. magnum had been reported from a number of sites in the South Island mountains, prior to our study, the only record of its presence on the North Island was from Mount Ruapehu on the central plateau and on Mount Taranaki [
32]. Its primarily South Island distribution, and apparent restriction to high mountain regions in North Island, suggest
D. magnum is particularly vulnerable to future climate warming.
Oniscigaster distans is also primarily a South Island species, although more widely distributed there than
D. magnum [
32,
57]. However, in the North Island, it also appears to be uncommon and, of only 10 distribution records, 4 were obtained in the present study. With one exception, these records are all from mountainous regions [
32] where stream water can be expected to be cooler at higher than at lower elevations. In contrast to the high-altitude and South Island species, mayflies currently confined to the warmer waters in northern New Zealand could also be at risk of at least local extinction if elevated water temperatures induce physiological stress, potentially leading to reductions in the size and extent of populations. The distribution of Ephemeroptera within New Zealand has undoubtedly changed markedly over many millennia as the geomorphology and climate of the country has evolved [
61]. Our snapshot of their present distribution provides a baseline for the subsequent evaluations in a time of rapid climate change.