Skip to main content
Ambio logoLink to Ambio
. 2019 Apr 27;49(3):704–717. doi: 10.1007/s13280-019-01185-y

Circumpolar terrestrial arthropod monitoring: A review of ongoing activities, opportunities and challenges, with a focus on spiders

Mark A K Gillespie 1,, Matthias Alfredsson 2, Isabel C Barrio 3,4, Joe Bowden 5,6, Peter Convey 7, Stephen J Coulson 8, Lauren E Culler 9,10, Martin T Dahl 11, Kathryn M Daly 12, Seppo Koponen 13, Sarah Loboda 14, Yuri Marusik 15,16, Jonas P Sandström 8, Derek S Sikes 12, Jozef Slowik 12, Toke T Høye 5,17
PMCID: PMC6989709  PMID: 31030417

Abstract

The terrestrial chapter of the Circumpolar Biodiversity Monitoring Programme (CBMP) has the potential to bring international multi-taxon, long-term monitoring together, but detailed fundamental species information for Arctic arthropods lags far behind that for vertebrates and plants. In this paper, we demonstrate this major challenge to the CBMP by focussing on spiders (Order: Araneae) as an example group. We collate available circumpolar data on the distribution of spiders and highlight the current monitoring opportunities and identify the key knowledge gaps to address before monitoring can become efficient. We found spider data to be more complete than data for other taxa, but still variable in quality and availability between Arctic regions, highlighting the need for greater international co-operation for baseline studies and data sharing. There is also a dearth of long-term datasets for spiders and other arthropod groups from which to assess status and trends of biodiversity. Therefore, baseline studies should be conducted at all monitoring stations and we make recommendations for the development of the CBMP in relation to terrestrial arthropods more generally.

Electronic supplementary material

The online version of this article (10.1007/s13280-019-01185-y) contains supplementary material, which is available to authorised users.

Keywords: Bioindicators, Climate change drivers, Community composition, Surrogates for biodiversity

Introduction

The pressing need for arthropod monitoring and baseline surveys in the Arctic has been emphasised numerous times, particularly given the likelihood of future widespread and rapid environmental changes (Danks 1992; Hodkinson and Jackson 2005; Christensen et al. 2013; Hodkinson et al. 2013; Coulson et al. 2014). Arthropods are responsible for, and central to, a host of ecological processes in polar habitats at a range of scales, such as pollination, decomposition and soil nutrient cycling (Gillespie et al. 2019). However, insights into temporal changes in the ecosystem services provided by this group of organisms will depend on high-quality data gathered over time (Lindenmayer and Likens 2010, Hodkinson et al. 2013). Furthermore, it is argued that connecting and standardising national biodiversity monitoring programmes across the northern circumpolar region would be cost-effective, allow for more timely management, and provide greater power to detect change (Christensen et al. 2013).

The Terrestrial Plan of the Circumpolar Biodiversity Monitoring Programme (CBMP; Christensen et al. 2013) aims to meet these challenges, setting out a framework to harmonise terrestrial species monitoring efforts across the Arctic. In this paper, we reiterate the need for greater support for the establishment of arthropod monitoring programmes within the CBMP due to large gaps in current knowledge. We begin by outlining the status of arthropod monitoring in the Arctic in general, and then use spiders as a model taxonomic group to further illustrate the challenges and opportunities of Arctic biomonitoring. Spiders are an ideal group for this purpose because they are a relatively well-studied, diverse and abundant group of arthropods, occurring in a range of Arctic habitats (Bowden and Buddle 2010a). By focusing on spiders, we can identify data deficiencies and needs that are likely to be relevant to most major groups of arthropods in the Arctic.

Why are arthropods important to monitor?

Long-term ecological monitoring is an important part of the commitment to reverse global biodiversity losses, partly because monitoring data help distinguish between diversity and abundance trends and natural fluctuations (Rohr et al. 2007). Yet many monitoring programmes suffer from bias in favour of charismatic and popular species groups such as birds, mammals, and flowering plants (Rohr et al. 2007; Hodkinson et al. 2013). In the Arctic, relatively good monitoring networks and baseline data exist for these groups (e.g. Elrich et al. this issue; Russel et al., this issue; Smith et al., this issue), but we lack similar fundamental information for arthropods (Hodkinson et al. 2013; Gillespie et al. 2019). Paradoxically, arthropods represent one of the most diverse groups, driving many of the ecosystem functions that require safeguarding such as nutrient cycling, decomposition and pollination (Hodkinson and Jackson 2005; Lavelle et al. 2006; Tiusanen et al. 2016; Koltz et al. 2017; Høye and Culler 2018). While the CBMP represents an opportunity to monitor arthropods alongside vertebrates and plants, detailed distribution and biological information is lacking for many species (Hodkinson et al. 2013).

The need for balanced monitoring is increasingly apparent due to the likelihood of strong arthropod responses to climate changes (Høye and Forchhammer 2008a; Høye et al. 2014; Loboda et al. 2018). Being ectothermic organisms with rapid developmental rates, relatively short generation times and often precise habitat requirements (e.g. soil moisture, vegetation cover), arthropods are sensitive to rapid climate change in the Arctic (Høye and Forchhammer 2008a). They can also provide the earliest indication of altered ecological systems (Danks 1992). For example, global temperature changes have already altered the phenology of invertebrates as food for mammals and birds (Tulp and Schekkerman 2008), and earlier snowmelt, and earlier and warmer springs have also affected the sexual dimorphism of the wolf spider Pardosa glacialis in Zackenberg, north-east Greenland (Høye et al. 2009).

While some species may actually benefit from climatic changes, as they may become less stressed or limited by cold conditions and short seasons, the effects of new interactions arising from range expansions are harder to predict (Convey 2011). The extent to which northward and elevational range shifts are already occurring is unknown due to the lack of research tracking distributional limits of species, but palaeo-ecological work has identified previous rapid shifts of invertebrate faunas in response to climate change (Elias et al. 2006). Poleward invertebrate range expansions will differ in nature for each region of the Arctic due to varying levels of geographical isolation. For example, species on isolated islands, such as Greenland, Iceland and Svalbard, have limited dispersal opportunities. Available transport routes and suitable habitats will also limit the arrival of species in these locations (Ingimarsdóttir et al. 2013). Furthermore, certain species are more adept at dispersing than others (Coulson et al. 2002, 2003) and the ability to survive in a new habitat and disperse further will vary between species (Hodkinson et al. 2013). Colonisation success will depend on factors such as micro-habitat structure and temperature, snowmelt and freeze/thaw cycles, the availability of moisture and species interactions (Hodkinson and Bird 1998; Bale and Hayward 2010). These factors themselves are likely to be subject to change, as shrub encroachment is expected to alter habitat structure, and early spring onset will alter phenological cues of some species and the timing of moisture availability (Cooper 2014).

Knowledge gaps in the monitoring of Arctic arthropods

A review of invertebrate monitoring approaches by Rohr et al. (2007) highlighted the need for structured inventories (i.e. species lists with relative abundances) and the identification of reliable “surrogates of biodiversity”. The diversity of these surrogate groups and how it changes over time may be indicative of broader biodiversity patterns. Identifying such taxa is important, therefore, because complete monitoring of a group as species-rich as the invertebrates is impractical using current, traditional methods. The CBMP adopts these approaches to a certain extent, outlining five large functional species groups of arthropods to target and report on, called Focal Ecosystem Components (FECs: pollinators, decomposers, prey for vertebrates, blood-feeding and herbivores). However, the FEC approach is difficult to implement for arthropods in practice. Categorisation is challenging for species performing multiple roles or where ecological information is scarce, and the approach underestimates the intensity of labour required to monitor ecological functions and identify sampled species (Gillespie et al. 2019). Furthermore, complete circumpolar inventories do not exist and, where country- or region-level inventories are available (e.g. Coulson et al. 2014; Böcher et al. 2015), the relative importance or abundance of species within communities and their correlations with functional biodiversity are only known for a few key sites (e.g. Cameron and Buddle 2017; Dahl et al. 2018; Koltz et al. 2018; Loboda et al. 2018).

Published work reporting long-term, extensive sampling is also limited in its species-level information (Høye and Forchhammer 2008a; Tulp and Schekkerman 2008; Bolduc et al. 2013), taxonomic coverage or geographic location/extent (Table 1, Fig. 1). Perhaps the most promising current multi-taxon monitoring programme for terrestrial arthropods is in Greenland. The Greenland Ecosystem Monitoring (GEM) Programme has been monitoring arthropods as well as plants, birds and mammals at Zackenberg (74°28′N, 20°34′W; Hansen et al. 2017) and Nuuk (64°08′N, 51°23′W; Topp-Jørgensen et al. 2017) since 1996 and 2008, respectively. Arthropods are sampled weekly during the growing season using pitfall and flight-intercept traps, and samples are sorted to family-level taxonomic resolution. Further species-level identification and analysis suggest abundance declines for some individual species (Bowden et al. 2018; Loboda et al. 2018) and diversity declines for some functional groups (Gillespie et al. 2019), but the data demonstrate high temporal and spatial (among habitat) variability.

Table 1.

Summary of the Arctic research stations currently involved in monitoring of arthropods

Country/state Location CAVM zone Year started Methods of annual invertebrate sampling Comments References
Alaska Toolik LTER Low Arctic 1980 Pitfall traps, CO2 traps from 2017 Short term projects only prior to 2017. NEON site status since 2017. Target species are ground beetles and mosquitoes. Other species stored as by-catch. Hobbie et al. (2003)
Utqiaġvik (Barrow) High Arctic 2015 Pitfall traps, CO2 traps NEON site since 2017. Target species as for Toolik Thorpe et al. (2016)
Canada CHARS, Cambridge Bay, Nunavut High Arctic Expected 2019 As CBMP One of the first CBMP stations Government of Canada (2018)
Bylot Island High Arctic 2005 Modified pitfall traps As part of broader ecosystem monitoring http://www.cen.ulaval.ca/bylot/ecomon-anispec-arthropod.htm
Greenland Zackenberg Ecological Research Operations High Arctic 1996 Pitfall traps, flight interception traps Weekly sampling, family-level identification Hansen et al. (2017)
Nuuk Ecological Research Operations Low Arctic 2008 Topp-Jørgensen et al. (2017)
Narsarsuaq Sub-Arctic 2014 Pitfall traps, Malaise traps Weekly sampling, some species-level identification (Høye et al. 2018)
Kangerlussuaq Low Arctic 2011 CO2 traps, Sweep nets, Bug vacs, Pitfall traps Mosquito monitoring since 2011; Terrestrial studies since 2015 Culler et al. (2015)
Iceland Surtsey Sub-Arctic 1967 Pitfall traps (from 2002), Malaise traps (from 2008) Baldursson and Ingadóttir (2006)
Mývatn Sub-Arctic 1977 Window traps Chironomidae and Simuliidae larval studies (Freshwater). See also moth survey sites (Sect. 5). Ives et al. (2008)
Rif Low Arctic 2017 Pitfall traps, Malaise traps One of the first CBMP stations Jóhannsdóttir et al. (2014)
Norway Varanger Sub-Arctic 2005 Survey transects Annual geometrid moth surveys Ims et al. (2013)
2011 Flight interception traps Annual saproxylic insect trapping. Station also located in Svalbard but arthropod monitoring is not conducted
Sweden Abisko Scientific Research Station Sub-Arctic 2003 Malaise trap Extensive study of all species. Short term project to 2005, may be resumed. Karlsson et al. (2005)
Finland Kevo Research Station Sub-Arctic 1972 Light traps Moth monitoring Kozlov et al. (2010)
Kilpisjärvi Biological Station Sub-Arctic 1993 Light traps Moth monitoring Välimäki et al. (2011)

Fig. 1.

Fig. 1

Circumpolar map indicating the locations of research stations with current or expected future arthropod monitoring activities. Details of the stations are in Table 1

Elsewhere, evidence of long-term trends comes from stand-alone studies, but these typically cover specific taxonomic groups such as moths (unpublished data, see Gillespie et al. 2019) and chironomids in Iceland (Ives et al. 2008), or recent repeats of historic surveys. For example, between 1947 and 1962, the Northern Insect Survey of Canada sampled insect diversity, with an initial focus on biting flies, at over 70 sites in the Canadian and Alaskan Arctic and sub-Arctic (Freeman 1959, Riegert 1999). More recent efforts through individual research programmes aimed to document changes in diversity (Buddle et al. 2008), although the lack of standardised sampling in the earlier surveys prevented the analysis of temporal trends for most species groups (but see Timms et al. 2013). Nevertheless, survey updates carried out in other regions may form the best source of information on “status and trends” of arthropods.

Further opportunities for generating long-term data exist through linking arthropod monitoring activities to programmes for other taxonomic groups. For example, throughout Canada and Alaska the Arctic Shorebird Demographics Network has been collecting terrestrial arthropods via pitfall trapping for nearly a decade. However, this programme is currently not linked to arthropod experts and the majority of samples have been dried for biomass sampling (e.g. Bolduc et al. 2013) to generate a gross estimate of food availability for birds. Long-term ecological research stations (e.g. INTERACT 2015) could also be expanded to include more arthropod sampling, by securing the resources to collect samples using standardised methods over long periods and identify them to species level. For example, invertebrates have been studied at the Long-Term Ecological Research Site, Toolik Field Station, located in the Brooks Range, North Slope of Alaska (e.g. Sikes et al. 2013; Koltz et al. 2017), but the station lacks a complete species-level inventory and historic long-term invertebrate monitoring dataset. Nevertheless, Toolik Field Station and the station at Utqiaġvik (Barrow) have recently been included in the U.S. National Ecological Observatory Network (NEON), a large-scale U.S. National Science Foundation project aiming to document ecological changes across the U.S. over the next three decades, incorporating pitfall and CO2 traps for arthropods (Thorpe et al. 2016). It is essential that such projects maintain these commitments and incorporate the standardised protocols of the CBMP in order to create useful baseline summaries. Further, funding to support DNA identification of the high volume of samples from these stations would contribute significantly to the timeliness and efficiency of biodiversity assessments, as well as provide other meaningful information such as improved reference sequences and detection of speciation processes (Porter and Hajibabaei 2018). Scientific engagement with, and productivity from, these types of sites is considered vital to the sustainability of monitoring programmes, because it ensures statistical rigour in sampling designs and facilitates a flow of communication between stakeholders, providing continued relevance of the programme (Lindenmayer and Likens 2010). More of these types of collaboration can close some of the enormous geographic gaps in the coverage of monitoring in the Arctic (Fig. 1). The few stations with current monitoring of arthropods found in the literature and on the internet (Table 1) are heavily biased towards insular Arctic, with few monitoring activities of note in continental Europe or Russia. Similarly, there is a latitudinal imbalance, with most monitoring occurring south of 70°N. While this list of stations is not exhaustive, and is not indicative of research or sampling effort (Metcalfe et al. 2018), it illustrates an alarming lack of coordinated efforts in arthropod monitoring.

Case study: Status and trends in Arctic spider diversity and abundance

Spiders are an excellent candidate group for focused monitoring in the Arctic, not only due to their ubiquity but also because they tend to be relatively easy to collect in a standardised manner (e.g. with pitfall traps, although this can bias the sample towards wandering species), are large enough for non-specialist researchers to separate to “morphotypes”, and unlike many other groups, all life stages perform similar functions and occur in the same habitats. In relation to the FEC classification system of the CBMP (Gillespie et al. 2019), spiders represent a large part of one of the FECs (prey for vertebrates). However, spiders are also pivotal in Arctic food webs, serving as the dominant terrestrial arthropod predators with the potential to reflect subtle ecosystem changes (Hodkinson and Coulson 2004; Wirta et al. 2015, Schmidt et al. 2018) and even environmental pollution (Jung and Lee 2012). Recent work has shown that molecular identification of spider prey from gut contents reflects the composition of the local community and prey availability (Schmidt et al. 2018). When DNA metabarcoding methodologies are incorporated within monitoring programmes, groups of organisms such as spiders may be important as “traps within traps”, providing rapid assessments of community composition and trophic cascades of environmental changes. This form of monitoring may be biased, however, as some spider species may prefer certain prey groups (Eitzinger et al. 2019).

In this case study, we begin by collating spider inventories for each Arctic region. We then summarise the current monitoring programmes that target spiders, and identify opportunities for more extensive sampling, before outlining key trends in, and drivers of, Arctic spider diversity. We conclude with recommendations for addressing important knowledge gaps and developing arthropod monitoring within the CBMP. It is hoped that, through illustrating the amount of work required for a relatively well-known group, this study will alert policy makers, funding agencies and other stakeholders to the need for far greater support for arthropod biodiversity initiatives more generally.

An inventory of circumpolar Araneae

The main aim of this section is to summarise the species richness of spiders for each country with land in the High-, Low-, and/or Sub-Arctic zones as defined by the Circumpolar Arctic Vegetation Map (CAVM; CAVM Team 2003), but with Sub-Arctic restricted to alpine habitats (i.e. those occurring above the treeline). Subsequently, we aim to highlight aspects of data quality and availability that will need to be addressed in future monitoring efforts. Full details of data sources and geographic classification can be found in the supplementary material. Species lists are given in Table S1.

We encountered two key issues in producing our summaries of species richness of Arctic spider families (Fig. 2, Table 2). First, much of the available information on species distribution is organised according to definitions other than the CAVM zones. For example, Marusik and Eskov (2009) provide a comprehensive list of species occurring in the Russian tundra, but the study reports on surveys across the CAVM High/Low Arctic boundary. Records in this and other studies are not digitised with geographic coordinates, preventing a classification of species by CAVM zones without direct examination of the specimens’ labels. The Russian richness value is therefore an underestimate, with significant regions such as Siberia largely omitted from consideration, and the figure representing the “Russian Arctic” as a whole. Second, species records are not always accompanied by elevation information, causing difficulties with classifying species as “alpine” (See Supplementary Material S1, S2). It was not possible to distinguish between alpine and non-alpine species in Canada at all, resulting in an inflated final richness value. Conversely, the species richness of the sub-Arctic alpine region of Alaska was estimated as only three species, based on assumptions of timberline elevation. This is clearly an underestimate and highlights the need for more alpine sampling and future recording of sampling elevations. Such information would particularly help to monitor species’ elevational range shifts.

Fig. 2.

Fig. 2

The diversity of the main spider families in the circumpolar region (those present in seven or more regions; the Other category consists of 10 families—see Table 2; note Franz Josef Land with only two Linyphiidae species is omitted for clarity). The size of the pie charts corresponds to the total richness of each area (see Table 2). Note that species richness for sub-Arctic regions consists only of alpine species, except for Canada, which includes both alpine and non-alpine species. The red dots indicate monitoring stations that target arthropods (Fig. 1, Table 1), but with those not using techniques to capture spiders removed

Table 2.

The number of spider species within each family and region of the circumpolar Arctic

graphic file with name 13280_2019_1185_Tab2_HTML.jpg

*This record refers to Titanoeca nivalis, found in the Oglivie mountains, Yukon (Bowden and Buddle 2010a, b), and northern Finland (Koponen et al. 2013)

Due to the above issues, we are restricted to broad inferences about diversity patterns. As expected, larger territories of the Arctic accommodate a richer fauna, and as with many other arthropod groups, the species richness and number of families decrease with increasing latitude (Hodkinson et al. 2013). An additional clear pattern from the data is that the spider family Linyphiidae dominates the Arctic fauna, probably reflecting a combination of their effective dispersal and colonisation ability and their cold-hardiness (Kumschick et al. 2009; Convey et al. 2015; Loboda and Buddle 2018). The Lycosidae are also well represented in the Arctic, absent only from some High Arctic islands, and species within this family tend to be collected in high abundance in open areas such as the tundra (Bowden and Buddle 2010a; Loboda and Buddle 2018) or forest gaps (e.g. Buddle et al. 2000). The species richness of this group also tends to make up between 7 and 10% of spider communities in most Arctic habitats, making it a consistent indicator of overall diversity (Y. Marusik, pers. obs.). Conversely, the Salticidae is the most species-rich spider family globally but is not well represented in the Arctic. The reason for this is not clear, but phylogeographic work indicates that the family radiated mainly in the tropics (Hill and Richman 2009).

Current monitoring of Arctic spiders

Ideally, a complete account of circumpolar spider diversity would include recent trends of diversity or abundance, as this would enable identification of those species, habitats, or regions most at risk from future environmental changes. Such evaluations have not been completed previously: there are no red data list records for Arctic spiders due to a lack of data, and remarkably, the only dataset with more than 10 years of standardised observations is that from the Zackenberg monitoring programme. Spiders from these samples have recently been identified to species level and analyses have revealed that some species have declined significantly in abundance between 1996 and 2014 at Zackenberg (Fig. 3). Specifically, some habitat specialists (Collinsia thulensis and Erigone psychrophila, both Linyphiidae) have significantly declined in the region in response to warming and earlier spring onset over the 18-year period (Bowden et al. 2018). Erigone psychrophila, in particular, is associated with a fen habitat at Zackenberg that is undergoing rapid reductions in cover through altered snow dynamics and increased evapotranspiration (Schmidt et al. 2012). This species also appears to have declined in Svalbard (M. Dahl, pers. obs.). Many other species demonstrate highly variable patterns in abundance, particularly Erigone arctica, which appeared to be declining until 2010, after which the population seems to increase, highlighting the need for continuous and uninterrupted long-term species monitoring across multiple habitats.

Fig. 3.

Fig. 3

Abundance of individuals per trap across the snow-free season and for all habitats combined, from 1996 to 2014 at Zackenberg Research Station, North-East Greenland, separated by key spider species. Abundances have been calculated to control for trapping effort by calculating abundance per trap-day for each trap, and then multiplying this value by the total number of trap days for the site (85). Solid lines are linear regression lines, significant at the p < 0.05 level. (Redrawn with permission from Bowden et al. 2018)

There is excellent potential elsewhere for long-term data generation (Table 1). Monitoring programmes have recently been launched elsewhere in Greenland, including an ambitious dedicated arthropod monitoring programme launched in 2014 at Narsarsuaq, South Greenland, building on the GEM arthropod sampling manual, with additional spatial replication also covering elevational variation (Høye et al. 2018). Also, in Kangerlussuaq in western Greenland, arthropod monitoring with pitfall traps began in 2016 with plans to continue through to at least 2021. Traps in Kangerlussuaq are in operation for three weeks in July and cover a range of habitat types (wind-eroded areas, shrub, grass) at sites near (< 1–2.5 km) and far (25 km) from the Greenland Ice Sheet. However, these relatively new endeavours must be assured of continuous funding to ensure that (a) sampling is conducted over long and uninterrupted time scales, and (b) trap catches are continually identified and counted to generate the data in a timely manner. DNA barcoding techniques are now widely available to help with the second requirement (Porter and Hajibabaei 2018). Furthermore, such efforts need to be expanded to cover more areas of the Arctic, as the locations that currently use trapping techniques to capture spiders (pitfall traps and sweep netting) on a regular basis are mainly restricted to the insular and Low or Sub-Arctic zones (Fig. 2). For spiders, and other terrestrial arthropods, information on trends over time are insufficient to extrapolate findings to other habitats, species groups and regions of the Arctic.

Drivers of spider diversity and community composition

Under future warmer conditions, spider diversity and community composition may be expected to change in many areas through changing snowmelt dynamics and moisture availability (Bowden et al. 2018). Shrub encroachment into alpine and Low Arctic habitats is also likely to lead to changes in spider community composition (Rich et al. 2013; Høye et al. 2018). For example, many ground dwelling wolf spider (Lycosidae) species are found in high densities on the Arctic tundra, preferring high solar irradiation for basking, thermoregulation and incubating their eggs (Bowden and Buddle 2012; Loboda and Buddle 2018), and such conditions may become fragmented or limited with the encroachment of shrubs. Other bottom-up processes via factors such as changing plant health and diversity, vegetation structure (Bowden and Buddle 2010b; Hansen et al. 2016), moisture availability and their effects on herbivore prey will likely combine with direct impacts on physiology and activity in ways that are as yet unclear (e.g. Barrio et al. 2016; Koltz et al. 2018).

In addition, species may have distinct responses to changing temperatures and moisture regimes (e.g. Danks 1992; Hodkinson et al. 1998; Dahl et al. 2018). Differential responses between trophic levels (e.g. spiders and prey) have the potential to disrupt species interactions with consequences for diversity and community composition (Høye and Forchhammer 2008b; Høye et al. 2014, Gillespie et al. 2016). Most of these impacts are understood in relation to spring and summer temperatures, but changing winter temperatures may also influence responses of arthropods such as winter-active spiders (Koltz et al. 2018). Thus, future studies are needed that specifically focus on the impact of changing winter conditions on arthropod abundance and diversity (Bale and Hayward 2010). There is also a paucity of studies recording biological microclimates over long timescales, which are necessary both in terms of understanding the stresses faced by organisms, and in identifying even large-scale changes in active season length (see discussion in Convey et al. 2018). At least for biological responses in body size, phenology and abundance, it is fairly clear that these are likely linked to snowmelt timing and temperature (Høye and Forchhammer 2008b; Høye et al. 2009; Bowden et al. 2015; Loboda et al. 2018).

Recommendations for circumpolar arthropod monitoring

In general, the species lists and isolated long-term datasets of our illustrative example are insufficient to assess the status of, or recent changes in, spider diversity (Christensen et al. 2013; Gillespie et al. 2019). However, this data collation has highlighted key knowledge gaps and requirements that will inform the initial stages of spider monitoring, as well as more general arthropod sampling. First, we lack structured inventories of the vast majority of arthropod groups in many regions of the Arctic (Hodkinson et al. 2013; Gillespie et al. 2019). Second, the geographical coverage of monitoring and potential for long-term data generation is clearly unbalanced across much of the Arctic and, even where there is good coverage, more habitat types and ecosystems require study. Third, these imbalances inevitably result in a dearth of long-term trend information for even the best-known species groups. Without more structure and organisation in our information about terrestrial Arctic arthropods, we cannot confidently establish which taxa should be the targets of monitoring and how they should be most efficiently collected.

Spiders are a good candidate biodiversity “surrogate”, particularly the Lycosidae. This family is well represented in easily implemented pitfall trapping due to a wandering predatory habit increasing the probability of capture compared to the sit-and-wait behaviour of the Linyphiidae. The consistent diversity representation of this family across habitats and zones would also enable early detection of changes in community composition, especially if captures are combined with DNA metabarcoding. However, we advise against relying on (a) one taxonomic group as a biodiversity surrogate, (b) only one trapping technique, and (c) catches from one or a few locations and habitats. The CBMP aims to avoid points (a) and (b), but we recommend that monitoring plans are expanded to address point (c). For example, monitoring at any particular station should involve trapping in multiple locations at small physical scales to account for subtle variations in variables such as soil moisture (Cameron and Buddle 2017; Høye et al. 2018), habitat (Wyant et al. 2011; Ernst et al. 2016) and vegetation structure (Bowden and Buddle 2010a; Hansen et al. 2016; Høye et al. 2018). Similarly, trapping should be conducted at multiple time points to include seasonal variation (Bowden et al. 2018). Given the degree of habitat/structural specialisation among Arctic spiders, for example, it may also be prudent to monitor changes in habitat conditions, particularly as air temperatures taken at research stations may not accurately reflect conditions experienced by surface-dwelling and soil invertebrates (Convey et al. 2018).

Overall, extensive initial work will be required at each monitoring station of the CBMP to determine the appropriate sampling design given local habitat conditions, establish structured species inventories and evaluate the extent to which the station represents the diversity of species in the region. Subsequent work should also investigate how sampled species groups meet the requirements of bioindicators or surrogate species (e.g. ease of identification, locally abundant, representative of the community or FEC, indicative of environmental changes, Hodkinson and Jackson 2005). To these ends, it will be important to foster partnerships between researchers (particularly taxonomists) and local communities, ensure strong leadership at monitoring stations and secure continued funding. These aspects are key in ensuring that preserved samples of arthropods are not left to accumulate in storage or be discarded. Rather, they should be identified in a timely manner to the appropriate taxonomic level, curated in suitable repositories, and their data shared (e.g. via the Global Biodiversity Information Facility; gbif.org) to enable future re-examination and use to generate both monitoring and research outputs (Rohr et al. 2007; Lindenmayer and Likens 2010).

Future species inventories should also be digitised to give accessible reference databases of circumpolar invertebrate species, along with their morphological and functional traits and habitat requirements. Existing trait databases for invertebrates, such as SoilBioStore (soilbiostore.au.dk) and BETSI (betsi.cesab.org), could be used to derive FECs and other functional groupings more easily. Where the ecosystem role of a species is poorly known, the level of current knowledge will be indicated by missing trait information and FEC assignment. Monitoring efforts should also be accompanied by the production of DNA barcode data which, given funding for environmental DNA studies and considerable improvements in sequence database coverage, will help make monitoring easier for such a diverse and challenging species group (Porter and Hajibabaei 2018). For example, Alaska has begun production of a DNA Barcode library of Alaskan arthropods, which has so far resulted in DNA barcodes for 1748 species (Sikes et al. 2017). This online library has already been used in a number of studies, including diet analyses of birds (McDermott 2017) and a study using high-throughput sequencing methods to inventory terrestrial arthropods (Bowser et al. 2017). A similar co-ordination project for barcodes of polar invertebrates generally, PolarBOL (http://www.polarbarcoding.ca/), also promises to provide an efficient mapping and monitoring tool for biodiversity on a large scale. The extension of barcode libraries of this kind to more species groups would be invaluable to the science of ecology and to broad monitoring programmes like the CBMP, particularly if samples cannot be identified by traditional means within reasonable time limits, or if sampling is incidental to monitoring of other groups such as mammals and birds. However, it should be noted that DNA-based methods should not replace traditional specimen-vouchering methods which support taxonomic research, particularly as some taxa cannot yet be identified by DNA barcodes (Rix et al. 2018), and as intact specimens provide important information for other valuable areas of study, such as intraspecific trait variation (Bowden et al. 2015).

Conclusion

In this review, we have demonstrated that the CBMP faces a huge challenge in making its arthropod monitoring efficient. We have identified the following recommendations for arthropod monitoring within the CBMP:

  1. On a pan-Arctic scale, there is a need to address the geographical imbalance in knowledge and monitoring of Arctic arthropods by prioritising the development of new monitoring stations in High Arctic locations, and maintaining existing stations.

  2. At local scales, initial studies are required at each station to create “structured inventories” (species lists with relative abundances), and to identify key surrogates for biodiversity in order to place monitoring data into context.

  3. The above initial studies should also provide local information on the habitat types to include in monitoring, and the specifics of the sampling regime (i.e. the timing and the types of methodologies used), to ensure target taxa are collected appropriately.

  4. Sampling programmes should be planned with rigorous statistical design and appropriate environmental monitoring (e.g. micro-habitat soil moisture and temperature) in order to link biological trends with environmental changes at biologically relevant scales (Convey et al. 2018).

  5. A detailed plan of continuous specimen identification and vouchering is required for each station, together with sustainable sources of funding set aside for taxonomic work and DNA barcoding, to ensure that samples are converted to usable, high-resolution, globally shared and open-access data.

The CBMP represents an unprecedented opportunity to bring knowledge of Arctic arthropods in line with that of their temperate counterparts, and ideally with that of vertebrates and flowering plants. It also has the potential to meet the pressing need for greater international collaboration, as is currently facilitated by the Network for Arthropods of the Tundra (Høye and Culler 2018) and the online sharing of open-access data. Much work and financial backing is required, however, if the programme is to come close to meeting its potential for arthropods.

Electronic supplementary material

Below is the link to the electronic supplementary material.

Acknowledgements

We thank Jukka Salmela for invaluable work during the initial phases of this study and Chris Buddle for early contributions to the CBMPs Invertebrate Expert Committee. Mikhail Kozlov, Armin Namayandeh, the special issue editor and two anonymous reviewers are also thanked for useful input. Thanks also to Hólmgrímur Helgason for preparation of Figs. 1 and 2. P. Convey is supported by NERC core funding to the BAS ‘Biodiversity, Evolution and Adaptation’ Team.

Biographies

Mark A. K. Gillespie

is an Associate Professor at the Western Norway University of Applied Sciences. His research interests include insect ecology and plant–insect interactions.

Matthias Alfredsson

is an Entomologist at the Icelandic Institute of Natural History. His research interests include Arctic insect ecology.

Isabel C. Barrio

is an Associate Professor at the Agricultural University of Iceland. Her research interests include tundra ecosystems and the role of Arctic invertebrate herbivory.

Joe Bowden

is a Research Scientist at the Natural Resources Canada, Canadian Forest Service. His research interests include northern arthropod ecology and climate change biology.

Peter Convey

is a Terrestrial Ecologist at the British Antarctic Survey. His research interests include polar ecosystems as models to identify the past and future global consequences of climate change and biogeography of polar terrestrial invertebrates, plants and microbes.

Stephen J. Coulson

is a Project Manager at the Swedish University of Agricultural Sciences. His research interests include ecology of terrestrial polar invertebrates including Arctic biogeography, dispersal, colonisation and ecosystem development, overwintering strategies (physiological and behavioural), Arctic invertebrate population dynamics and plant/insect interactions.

Lauren E. Culler

is a Research Assistant Professor at the Dartmouth College. Her research interests include the impacts of rapid environmental change on insect population and community dynamics in northern ecosystems.

Martin T. Dahl

is a Laboratory Technician at the FRAM Centre in Norway. His research interests include marine benthic and terrestrial invertebrate taxonomy and ecology.

Kathryn M. Daly

is a MS student at the University of Alaska Museum. Her research interests include the biogeography of Alaska’s butterflies and an examination of the historical data to assess if there is a climate change signal.

Seppo Koponen

is a Curator emeritus at the University of Turku. His research interests include Arachnology and Arctic ecology.

Sarah Loboda

is a PhD student at the McGill University. Her research interests include Arctic arthropod ecology and effects of climate change on invertebrate communities.

Yuri Marusik

is a Research Scientist at the Institute for Biological Problems of the North RAS. His research interests include taxonomy, distribution, palaeontology, ecophysiology and ecology of spiders.

Jonas P. Sandström

is an Environmental Analyst at the Swedish University of Agricultural Sciences. His research interests include terrestrial invertebrate ecology and taxonomy.

Derek S. Sikes

is a Professor and the curator of insects at the University of Alaska Museum. His research interests include taxonomy, morphological and molecular based phylogenetics, conservation, and arthropod faunistics, primarily of Coleoptera.

Jozef Slowik

is a Research Affiliate at the University of Alaska Museum. His research interests include spider taxonomy, life history, faunistics, and phylogeny, specifically the spider families Linyphiidae and Lycosidae.

Toke T. Høye

is Senior Researcher at the Aarhus University. His research interests include the effects of global change on populations of plants and animals. He leads the Network for Arthropods of the Tundra (NeAT).

Footnotes

Publisher's Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Contributor Information

Mark A. K. Gillespie, Email: markg@hvl.no

Matthias Alfredsson, Email: matti@ni.is.

Isabel C. Barrio, Email: isabel@lbhi.is

Joe Bowden, Email: joseph.bowden@canada.ca.

Peter Convey, Email: pcon@bas.ac.uk.

Stephen J. Coulson, Email: stephen.coulson@slu.se

Lauren E. Culler, Email: lauren.e.culler@dartmouth.edu

Martin T. Dahl, Email: MA_TO_DA@hotmail.com

Kathryn M. Daly, Email: kmdaly@alaska.edu

Seppo Koponen, Email: sepkopo@utu.fi.

Sarah Loboda, Email: sarah.loboda@gmail.com.

Yuri Marusik, Email: yurmar@mail.ru.

Jonas P. Sandström, Email: Jonas.Sandstrom@slu.se

Derek S. Sikes, Email: dssikes@alaska.edu

Jozef Slowik, Email: slowspider@gmail.com.

Toke T. Høye, Email: tth@bios.au.dk

References

  1. Baldursson S, Ingadóttir AI, editors. Nomination of Surtsey for the UNESCO World Heritage List. Reykjavik: Icelandic Institute of Natural History; 2006. [Google Scholar]
  2. Bale JS, Hayward SAL. Insect overwintering in a changing climate. Journal of Experimental Biology. 2010;213:980–994. doi: 10.1242/jeb.037911. [DOI] [PubMed] [Google Scholar]
  3. Barrio IC, Bueno CG, Hik DS. Warming the tundra: Reciprocal responses of invertebrate herbivores and plants. Oikos. 2016;125:20–28. [Google Scholar]
  4. Böcher J, Kristensen NP, Pape T, Vilhelmsen L, editors. The Greenland entomofauna: An identification manual of insects, spiders and their allies. Leiden: Koninklijke Brill nv; 2015. [Google Scholar]
  5. Bolduc E, Casajus N, Legagneux P, McKinnon L, Gilchrist HG, Leung M, Morrison RIG, Reid D, et al. Terrestrial arthropod abundance and phenology in the Canadian Arctic: Modelling resource availability for Arctic-nesting insectivorous birds. Canadian Entomologist. 2013;145:155–170. [Google Scholar]
  6. Bowden JJ, Buddle CM. Determinants of ground-dwelling spider assemblages at a regional scale in the Yukon Territory, Canada. Ecoscience. 2010;17:287–297. [Google Scholar]
  7. Bowden JJ, Buddle CM. Spider assemblages across elevational and latitudinal gradients in the Yukon Territory, Canada. Arctic. 2010;63:261–272. [Google Scholar]
  8. Bowden JJ, Buddle CM. Life history of tundra-dwelling wolf spiders (Araneae: Lycosidae) from the Yukon Territory, Canada. Canadian Journal of Zoology-Revue Canadienne De Zoologie. 2012;90:714–721. [Google Scholar]
  9. Bowden JJ, Eskildsen A, Hansen RR, Olsen K, Kurle CM, Hoye TT. High-Arctic butterflies become smaller with rising temperatures. Biology Letters. 2015;11:20150574. doi: 10.1098/rsbl.2015.0574. [DOI] [PMC free article] [PubMed] [Google Scholar]
  10. Bowden JJ, Hansen OLP, Olsen K, Schmidt NM, Høye TT. Drivers of inter-annual variation and long-term change in High-Arctic spider species abundances. Polar Biology. 2018;41:1635–1649. doi: 10.1007/s00300-018-2351-0. [DOI] [Google Scholar]
  11. Bowser ML, Morton JM, Hanson JD, Magness DR, Okuly M. Arthropod and oligochaete assemblages from grasslands of the southern Kenai Peninsula, Alaska. Biodiversity Data Journal. 2017;5:e10792. doi: 10.3897/BDJ.5.e10792. [DOI] [PMC free article] [PubMed] [Google Scholar]
  12. Buddle, C. M., D. C. Currie, and D. Giberson. 2008. Northern insect survey, 63–64. Newsletter of the Biological Survey of Canada (Terrestrial Arthropods).
  13. Buddle CM, Spence JR, Langor DW. Succession of boreal forest spider assemblages following wildfire and harvesting. Ecography. 2000;23:424–436. [Google Scholar]
  14. Cameron ER, Buddle CM. Seasonal change and microhabitat association of Arctic spider assemblages (Arachnida: Araneae) on Victoria Island (Nunavut, Canada) Canadian Entomologist. 2017;149:357–371. [Google Scholar]
  15. CAVM Team, C. 2003. Circumpolar Arctic vegetation map. Scale 1:7,500,000. Conservation of Arctic Flora and Fauna (CAFF) Map No. 1. U.S. Fish and Wildlife Service, Anchorage.
  16. Christensen, T., J. Payne, M. Doyle, G. Ibarguchi, J. Taylor, N.M. Schmidt, M. Gill, M. Svoboda, et al. 2013. The Arctic terrestrial biodiversity monitoring plan. 7, CAFF International Secretariat. Akureyri, Iceland.
  17. Convey P. Antarctic terrestrial biodiversity in a changing world. Polar Biology. 2011;34:1629. [Google Scholar]
  18. Convey P, Abbandonato H, Bergan F, Beumer LT, Biersma EM, Brathen VS, D’Imperio L, Jensen CK, et al. Survival of rapidly fluctuating natural low winter temperatures by High Arctic soil invertebrates. Journal of Thermal Biology. 2015;54:111–117. doi: 10.1016/j.jtherbio.2014.07.009. [DOI] [PubMed] [Google Scholar]
  19. Convey P, Coulson SJ, Worland MR, Sjöblom A. The importance of understanding annual and shorter-term temperature patterns and variation in the surface levels of polar soils for terrestrial biota. Polar Biology. 2018;41:1587–1605. [Google Scholar]
  20. Cooper EJ. Warmer shorter winters disrupt Arctic Terrestrial Ecosystems. Annual Review of Ecology Evolution and Systematics. 2014;45:271–295. [Google Scholar]
  21. Coulson SI, Hodkinson ID, Webb NR. Microscale distribution patterns in high Arctic soil microarthropod communities: The influence of plant species within the vegetation mosaic. Ecography. 2003;26:801–809. [Google Scholar]
  22. Coulson SJ, Convey P, Aakra K, Aarvik L, Avila-Jimenez ML, Babenko A, Biersma EM, Bostrom S, et al. The terrestrial and freshwater invertebrate biodiversity of the archipelagoes of the Barents Sea, Svalbard, Franz Josef Land and Novaya Zemlya. Soil Biology & Biochemistry. 2014;68:440–470. [Google Scholar]
  23. Coulson SJ, Hodkinson ID, Webb NR, Harrison JA. Survival of terrestrial soil-dwelling arthropods on and in seawater: Implications for trans-oceanic dispersal. Functional Ecology. 2002;16:353–356. [Google Scholar]
  24. Culler LE, Ayres MP, Virginia RA. In a warmer Arctic, mosquitoes avoid increased mortality from predators by growing faster. Proceedings of the Royal Society B-Biological Sciences. 2015;282:20151549. doi: 10.1098/rspb.2015.1549. [DOI] [PMC free article] [PubMed] [Google Scholar]
  25. Dahl MT, Yoccoz NG, Aakra K, Coulson SJ. The Araneae of Svalbard: The relationships between specific environmental factors and spider assemblages in the High Arctic. Polar Biology. 2018;41:839–853. [Google Scholar]
  26. Danks HV. Arctic insects as indicators of environmental-change. Arctic. 1992;45:159–166. [Google Scholar]
  27. Eitzinger B, Abrego N, Gravel D, Huotari T, Vesterinen EJ, Roslin T. Assessing changes in arthropod predator–prey interactions through DNA-based gut content analysis—variable environment, stable diet. Molecular Ecology. 2019;28:266–280. doi: 10.1111/mec.14872. [DOI] [PubMed] [Google Scholar]
  28. Elias SA, Kuzmina S, Kiselyov S. Late Tertiary origins of the Arctic beetle fauna. Palaeogeography, Palaeoclimatology, Palaeoecology. 2006;241:373–392. [Google Scholar]
  29. Ernst CM, Loboda S, Buddle CM. Capturing northern biodiversity: Diversity of arctic, subarctic and north boreal beetles and spiders are affected by trap type and habitat. Insect Conservation and Diversity. 2016;9:63–73. [Google Scholar]
  30. Freeman TN. The Canadian Northern Insect Survey, 1947–57. Polar Record. 1959;9:299–307. [Google Scholar]
  31. Gillespie MAK, Baggesen N, Cooper EJ. High Arctic flowering phenology and plant-pollinator interactions in response to delayed snow melt and simulated warming. Environmental Research Letters. 2016;11:115006. doi: 10.1088/1748-9326/11/11/115006. [DOI] [Google Scholar]
  32. Gillespie MAK, Alfredsson M, Barrio IC, Bowden JJ, Convey P, Culler LE, Coulson SJ, Krogh PH, et al. Status and trends of terrestrial arthropod abundance and diversity in the North Atlantic region of the Arctic. Ambio. 2019 doi: 10.1007/s13280-019-01162-5. [DOI] [PMC free article] [PubMed] [Google Scholar]
  33. Government of Canada. 2018. The Canadian High Arctic Research Station (CHARS) campus.
  34. Hansen, J., E. Topp-Jørgensen, and T.R.E. Christensen. 2017. Zackenberg Ecological Research Operations 21st annual report, 2015. Aarhus University, DCE—Danish Centre for Environment and Energy.
  35. Hansen RR, Hansen OLP, Bowden JJ, Treier UA, Normand S, Høye TT. Meter scale variation in shrub dominance and soil moisture structure Arctic arthropod communities. PeerJ. 2016;4:e2224. doi: 10.7717/peerj.2224. [DOI] [PMC free article] [PubMed] [Google Scholar]
  36. Hill DE, Richman DB. The evolution of jumping spiders (Araneae: Salticidae): A review. Peckhamia. 2009;75:1–7. [Google Scholar]
  37. Hobbie JE, Carpenter SR, Grimm NB, Gosz JR, Seastedt TR. The US long term ecological research program. BioScience. 2003;53:21–32. [Google Scholar]
  38. Hodkinson, I.D., A. Babenko, V. Behan-Pelletier, J. Böcher, G. Boxshall, F. Brodo, S.J. Coulson, W.H. De Smet, et al. 2013. Terrestrial and freshwater invertebrates.In Arctic Biodiversity Assessment. Status and trends in Arctic biodiversity, ed. H.E.A. Meltofte. Conservation of Arctic Flora and Fauna, Akureyri.
  39. Hodkinson ID, Bird J. Host-specific insect herbivores as sensors of climate change in arctic and Alpine environments. Arctic and Alpine Research. 1998;30:78–83. [Google Scholar]
  40. Hodkinson ID, Coulson SJ. Are high Arctic terrestrial food chains really that simple? The Bear Island food web revisited. Oikos. 2004;106:427–431. [Google Scholar]
  41. Hodkinson ID, Jackson JK. Terrestrial and aquatic invertebrates as bioindicators for environmental monitoring, with particular reference to mountain ecosystems. Environmental Management. 2005;35:649–666. doi: 10.1007/s00267-004-0211-x. [DOI] [PubMed] [Google Scholar]
  42. Hodkinson ID, Webb NR, Bale JS, Block W, Coulson SJ, Strathdee AT. Global change and Arctic ecosystems: Conclusions and predictions from experiments with terrestrial invertebrates on spitsbergen. Arctic and Alpine Research. 1998;30:306–313. [Google Scholar]
  43. Høye TT, Bowden JJ, Hansen OLP, Hansen RR, Henriksen TN, Niebuhr A, Skytte MG. Elevation modulates how Arctic arthropod communities are structured along local environmental gradients. Polar Biology. 2018;41:1555–1565. [Google Scholar]
  44. Høye TT, Culler LE. Tundra arthropods provide key insights into ecological responses to environmental change. Polar Biology. 2018;41:1523–1529. [Google Scholar]
  45. Høye TT, Eskildsen A, Hansen RR, Bowden JJ, Schmidt NM, Kissling WD. Phenology of high-arctic butterflies and their floral resources: Species-specific responses to climate change. Current Zoology. 2014;60:243–251. [Google Scholar]
  46. Høye TT, Forchhammer MC. The influence of weather conditions on the activity of High-Arctic arthropods inferred from long-term observations. BMC Ecology. 2008;8:8. doi: 10.1186/1472-6785-8-8. [DOI] [PMC free article] [PubMed] [Google Scholar]
  47. Høye TT, Forchhammer MC. Phenology of high-arctic arthropods: Effects of climate on spatial, seasonal and inter-annual variation. Advances in Ecological Research. 2008;40:299–324. [Google Scholar]
  48. Høye TT, Hammel JU, Fuchs T, Toft S. Climate change and sexual size dimorphism in an Arctic spider. Biology Letters. 2009;5:542–544. doi: 10.1098/rsbl.2009.0169. [DOI] [PMC free article] [PubMed] [Google Scholar]
  49. Ims, RA., J.U. Jepsen, A. Stien, and N.G. Yoccoz, editors. 2013. Science plan for COAT: Climate-ecological observatory for Arctic Tundra Fram Centre by the University of Tromsø, Fram Centre by the University of Tromsø.
  50. Ingimarsdóttir M, Ripa J, Magnúsdóttir ÓB, Hedlund K. Food web assembly in isolated habitats: A study from recently emerged nunataks, Iceland. Basic and Applied Ecology. 2013;14:174–183. [Google Scholar]
  51. INTERACT . INTERACT Station catalogue—2015. Danish Centre for Environment and Energy. Aarhus: Aarhus University; 2015. [Google Scholar]
  52. Ives AR, Einarsson Á, Jansen VAA, Gardarsson A. High-amplitude fluctuations and alternative dynamical states of midges in Lake Myvatn. Nature. 2008;452:84–87. doi: 10.1038/nature06610. [DOI] [PubMed] [Google Scholar]
  53. Jung MP, Lee JH. Bioaccumulation of heavy metals in the wolf spider, Pardosa astrigera L. Koch (Araneae: Lycosidae) Environmental Monitoring and Assessment. 2012;184:1773–1779. doi: 10.1007/s10661-011-2077-8. [DOI] [PubMed] [Google Scholar]
  54. Jóhannsdóttir SS, Kolbeinsson Y, Þórarinsson ÞL. Rif Field Station report. Húsavík: NE Iceland Nature Centre; 2014. [Google Scholar]
  55. Karlsson D, Pape T, Johansson KA, Liljeblad J, Ronquist F. The Swedish Malaise trap project, or how many species of Hymenoptera and Diptera are there in Sweden? Entomologisk Tidsskrift. 2005;126:43–53. [Google Scholar]
  56. Koltz AM, Asmus A, Gough L, Pressler Y, Moore JC. The detritus-based microbial-invertebrate food web contributes disproportionately to carbon and nitrogen cycling in the Arctic. Polar Biology. 2017;41:1531–1545. [Google Scholar]
  57. Koltz AM, Schmidt NM, Høye TT. Differential arthropod responses to warming are altering the structure of Arctic communities. Royal Society Open Science. 2018;5:171503. doi: 10.1098/rsos.171503. [DOI] [PMC free article] [PubMed] [Google Scholar]
  58. Koponen, S., T. Pajunen, and N.R. Fritzén. 2013: Atlas of the Araneae of Finland. Finnish Expert Group on Araneae. http://biolcoll.utu.fi/arach/aran2013/aranmaps.htm.
  59. Kozlov MV, Hunter MD, Koponen S, Kouki J, Niemela P, Price PW. Diverse population trajectories among coexisting species of subarctic forest moths. Population Ecology. 2010;52:295–305. [Google Scholar]
  60. Kumschick S, Schmidt-Entling MH, Bacher S, Hickler T, Entling W, Nentwig W. Water limitation prevails over energy in European diversity gradients of sheetweb spiders (Araneae: Linyphiidae) Basic and Applied Ecology. 2009;10:754–762. [Google Scholar]
  61. Lavelle P, Decaëns T, Aubert M, Barot S, Blouin M, Bureau F, Margerie P, Mora P, Rossi JP. Soil invertebrates and ecosystem services. European Journal of Soil Biology. 2006;42:S3–S15. [Google Scholar]
  62. Lindenmayer DB, Likens GE. The science and application of ecological monitoring. Biological Conservation. 2010;143:1317–1328. [Google Scholar]
  63. Loboda S, Buddle CM. Small to large-scale patterns of ground-dwelling spider (Araneae) diversity across northern Canada. FACETS. 2018;3:880–895. [Google Scholar]
  64. Loboda S, Savage J, Buddle CM, Schmidt NM, Hoye TT. Declining diversity and abundance of High Arctic fly assemblages over two decades of rapid climate warming. Ecography. 2018;41:265–277. [Google Scholar]
  65. Marusik, Y.M., and K.Y. Eskov. 2009. Spiders (Arachnida: Aranei) of the tundra zone of Russia. In Species and communities in extreme environments, ed. S.I. Golovatch, O.L. Markarova, A.B. Babenko, and L.D. Penev. Pensoft Publishers & KMK Scientific Press, Sofia, Moscow.
  66. McDermott, M.T. 2017. Arthropod communities and passerine diet: Effects of shrub expansion in Western Alaska. Thesis (M.S.) University of Alaska Fairbanks, Alaska, US.
  67. Metcalfe DB, Hermans TDG, Ahlstrand J, Becker M, Berggren M, Björk RG, Björkman MP, Blok D, et al. Patchy field sampling biases understanding of climate change impacts across the Arctic. Nature Ecology & Evolution. 2018;2:1443–1448. doi: 10.1038/s41559-018-0612-5. [DOI] [PubMed] [Google Scholar]
  68. Porter TM, Hajibabaei M. Scaling up: A guide to high-throughput genomic approaches for biodiversity analysis. Molecular Ecology. 2018;27:313–338. doi: 10.1111/mec.14478. [DOI] [PubMed] [Google Scholar]
  69. Rich ME, Gough L, Boelman NT. Arctic arthropod assemblages in habitats of differing shrub dominance. Ecography. 2013;36:994–1003. [Google Scholar]
  70. Riegert, P. 1999. The Survey of Insects of Northern Canada 1947–1962. Rempeck Publ., SK, Entomological Series No. 8. 49 pp.
  71. Rix MG, Raven RJ, Austin AD, Cooper SJB, Harvey MS. Systematics of the spiny trapdoor spider genus Bungulla (Mygalomorphae: Idiopidae): Revealing a remarkable radiation of mygalomorph spiders from the Western Australian arid zone. Journal of Arachnology. 2018;46:249–344. [Google Scholar]
  72. Rohr JR, Mahan CG, Kim KC. Developing a monitoring program for invertebrates: Guidelines and a case study. Conservation Biology. 2007;21:422–433. doi: 10.1111/j.1523-1739.2006.00578.x. [DOI] [PubMed] [Google Scholar]
  73. Schmidt NM, Kristensen DK, Michelsen A, Bay C. High Arctic plant community responses to a decade of ambient warming. Biodiversity. 2012;13:191–199. [Google Scholar]
  74. Schmidt NM, Mosbacher JB, Eitzinger B, Vesterinen EJ, Roslin T. High resistance towards herbivore-induced habitat change in a high Arctic arthropod community. Biology Letters. 2018;14:20180054. doi: 10.1098/rsbl.2018.0054. [DOI] [PMC free article] [PubMed] [Google Scholar]
  75. Sikes DS, Draney ML, Fleshman B. Unexpectedly high among-habitat spider (Araneae) faunal diversity from the Arctic Long-Term Experimental Research (LTER) field station at Toolik Lake, Alaska, United States of America. Canadian Entomologist. 2013;145:219–226. [Google Scholar]
  76. Sikes DS, Bowser M, Morton JM, Bickford C, Meierotto S, Hildebrandt K. Building a DNA barcode library of Alaska’s non-marine arthropods. Genome. 2017;60:248–259. doi: 10.1139/gen-2015-0203. [DOI] [PubMed] [Google Scholar]
  77. Thorpe AS, Barnett DT, Elmendorf SC, Hinckley ELS, Hoekman D, Jones KD, LeVan KE, Meier CL, et al. Introduction to the sampling designs of the National Ecological Observatory Network Terrestrial Observation System. Ecosphere. 2016;7:e01627. [Google Scholar]
  78. Timms LL, Bennett AMR, Buddle CM, Wheeler TA. Assessing five decades of change in a High Arctic parasitoid community. Ecography. 2013;36:1227–1235. [Google Scholar]
  79. Tiusanen M, Hebert PDN, Schmidt NM, Roslin T. One fly to rule them all-muscid flies are the key pollinators in the Arctic. Proceedings of the Royal Society B-Biological Sciences. 2016;283:8. doi: 10.1098/rspb.2016.1271. [DOI] [PMC free article] [PubMed] [Google Scholar]
  80. Topp-Jørgensen, E., J. Hansen, and T.R.E. Christensen. 2017. Nuuk Ecological Research Operations 9th annual report, 2015. Aarhus University, DCE—Danish Centre for Environment and Energy.
  81. Tulp I, Schekkerman H. Has prey availability for arctic birds advanced with climate change? Hindcasting the abundance of tundra arthropods using weather and seasonal variation. Arctic. 2008;61:48–60. [Google Scholar]
  82. Välimäki P, Männistö K, Kaitila J-P. Katsaus Enontekiön uhanalaisiin tunturiperhoslajeihin ja tunturiperhosseurannan esiintymisaluehavaintoihin vuosina 2008–2011. Baptria. 2011;36:70–90. [Google Scholar]
  83. Wirta HK, Vesterinen EJ, Hambäck PA, Weingartner E, Rasmussen C, Reneerkens J, Schmidt NM, Gilg O, Roslin T. Exposing the structure of an Arctic food web. Ecology and Evolution. 2015;5:3842–3856. doi: 10.1002/ece3.1647. [DOI] [PMC free article] [PubMed] [Google Scholar]
  84. Wyant KA, Draney ML, Moore JC. Epigeal spider (Araneae) communities in moist acidic and dry heath tundra at Toolik Lake, Alaska. Arctic, Antarctic, and Alpine Research. 2011;43:301–312. [Google Scholar]

Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Supplementary Materials


Articles from Ambio are provided here courtesy of Springer

RESOURCES