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Review

A Secondary Analysis of Invasion Risk in the Context of an Altered Thermal Regime in the Great Lakes

1
Cooperative Institute for Great Lakes Research, Ann Arbor, MI 48109, USA
2
Michigan Sea Grant, University of Michigan, Ann Arbor, MI 48109, USA
3
Michigan Sea Grant, Michigan State University, East Lansing, MI 48824, USA
*
Author to whom correspondence should be addressed.
Diversity 2025, 17(12), 861; https://doi.org/10.3390/d17120861
Submission received: 27 October 2025 / Revised: 3 December 2025 / Accepted: 10 December 2025 / Published: 16 December 2025
(This article belongs to the Special Issue Climate Change and Invasive Species Impacts on Freshwater Systems)

Abstract

Invasive species and changing thermal structure are widely recognized as drivers of change to freshwater ecosystems, yet the interactions of these two drivers have rarely been studied. This study conducted a secondary analysis of a large federal database (GLANSIS) of literature used in assessing the current risk of potential nonindigenous species to the Great Lakes (watchlist species) to evaluate how increased water temperatures would impact the risk of establishment posed by these species. Our analysis found that 46% of the current watchlist species would pose a higher potential risk while 7% would pose a lower potential risk. Lake Superior and Lake Huron exhibited significant increases in the number of species likely to find a suitable habitat.

1. Introduction

Freshwater ecosystems worldwide have been deeply transformed by invasive species [1,2] and a growing body of literature from an array of freshwater ecosystems has detailed, categorized, and improved our understanding of the environmental and socioeconomic impact of invasive species on these systems [3,4,5,6]. Similarly, recent changes to climate are already documented to have affected freshwater systems worldwide [7], and projections indicate that, if left unchecked, these impacts are likely to accelerate over the next several decades [8,9,10,11,12]. However, studies of the intersections of these two key drivers of ecosystem change remain rare [13,14].
Containing 20% of the world’s fresh surface water, the Laurentian Great Lakes encompass an area of 240,000 square kilometers and sustain thousands of native fishes, invertebrates, plants, and other species that contribute not only to the region’s recreational and economic vitality, but also to its ecological integrity. With more than 180 aquatic nonindigenous species recorded, the Great Lakes basin is regarded as one of the most heavily invaded freshwater ecosystems globally [15,16,17,18]. Climate change is projected to have multiple complex impacts on the Great Lakes, including changes to air temperature [19], surface water temperature [20], precipitation [19], groundwater supply [21], water levels [22], stratification [23], ice cover [24], coastal habitats [25], and species composition [20]. Parallel to the global literature, studies focused on the interaction of climate and invasive species in the Great Lakes have been rare or narrowly focused in scope [26,27,28].
Secondary analysis is the process of reanalyzing existing data collected for other purposes to answer new research questions. Secondary analysis differs from a classic systematic review in that it addresses broader or entirely different review questions rather than specific hypotheses similar to the original papers; it typically relies on sources other than bibliographic databases; it may reinterpret data or conclusions in new contexts; and it may be iterative, revising review questions as new information is added [29]. Secondary analysis also differs from meta-analysis, which synthesizes the results of separate studies, but typically statistically re-analyzing data gathered from studies conducted using similar methods and for similar purposes [30]. Secondary analysis is particularly useful in ecological studies when combining different types of data gathered independently for separate purposes (e.g., species-specific thermal tolerance studies with thermal projections for future water temperatures) and when re-examining historic data in the context of new issues (such as the intersection of climate change and invasive species).
The objective of this research was to improve understanding of how changes to environmental temperatures impact invasion risk, specifically how previously identified invasion risk to the Great Lakes may alter in the future as water and air temperatures warm. This secondary analysis addresses the following questions: Which of the potential invasive species identified as a current risk to the Great Lakes are likely to pose a threat under projected changes to the thermal regime (under 2050 climate scenarios)? Which of these potential invasive species pose a higher (and lower) risk and what is the net change in risk for each species?

2. Materials and Methods

The geographic scope of this study was framed to the Laurentian Great Lakes (Figure 1) below the ordinary high water mark including ordinarily connected wetlands. It does not include information for inland lakes or streams of the larger basin. This study examines how projected changes to thermal parameters directly interact with species thermal tolerances to impact the probability of establishment for a subset of species pre-identified (by the National Oceanic and Atmospheric Administration, NOAA) as posing a potential threat for introduction and establishment under current conditions. This study does not include nonnative species already established in the Great Lakes.
Figure 1. Study area, Laurentian Great Lakes below the ordinary high water mark (bold black line on map). Data Layers: Great Lakes Basin boundary (source: Great Lakes Aquatic Habitat Framework—GLAHF, University of Michigan), U.S. states (source: Esri, U.S. Census Bureau, NOAA, NGS), world countries (source: Esri, Garmin, U.S. Central Intelligence Agency). Inset map included for geographic context with the red box indicating the area of the detailed map.
Figure 1. Study area, Laurentian Great Lakes below the ordinary high water mark (bold black line on map). Data Layers: Great Lakes Basin boundary (source: Great Lakes Aquatic Habitat Framework—GLAHF, University of Michigan), U.S. states (source: Esri, U.S. Census Bureau, NOAA, NGS), world countries (source: Esri, Garmin, U.S. Central Intelligence Agency). Inset map included for geographic context with the red box indicating the area of the detailed map.
Diversity 17 00861 g001
We used information compiled by Great Lakes Aquatic Nonindigenous Species Information System (GLANSIS), including watchlist species risk assessments (available at https://www.glerl.noaa.gov/glansis/assessments/ (accessed on 20 May 2025) as well as in the appendices of NOAA GLERL Technical Memoranda [31,32,33,34,35,36]) and GLANSIS Watchlist species profiles (available at https://www.glerl.noaa.gov/glansis/ (accessed on 20 May 2025)). In cooperation with USGS, NOAA’s Great Lakes Environmental Research Laboratory (GLERL) has been tracking nonindigenous aquatic species in the Great Lakes system since 2003 and serving that information through the GLANSIS database [31]. Information in the database includes an overview of the species life history, ecology, and invasion history, comprehensive risk assessment, and overview of management options. All GLANSIS assessments and profiles were developed by NOAA staff and affiliates and subject to external expert review prior to NOAA publication. The GLANSIS criteria for inclusion of species in the watchlist include the following:
Geographic criterion: Lives in a known donor region (such as rivers adjacent to Great Lakes, inland lakes in the Great Lakes region, western Europe, the Ponto-Caspian region) or in a zone with high specialization, species pool, or climate conditions that match the Great Lakes.
Aquatic criterion: GLANSIS includes only aquatic species spending most of their life cycle below water. USDA wetland indicator status is used as a guideline for determining whether wetland plants should be included in the list—Obligate, Facultative Wetland, and Facultative plants are included in this list as aquatic; Facultative Upland and Upland plants are not. GLANSIS does not include mammals or birds but does include amphibians and turtles.
Establishment criterion: Not already established in the Great Lakes, but assessed as ‘likely’ to become so in peer-reviewed literature or via our assessment [32,37] as follows:
  • Vector Subcriterion: A transport vector currently exists that could move the species into the Great Lakes. The species is likely to tolerate/survive transport (including in resting stages) in the identified vector. The species has a probability of being introduced multiple times or in large numbers.
  • Reproduction and Overwintering Subcriterion: In addition, based on known tolerances or climate matching, the species is likely to be able to successfully reproduce and overwinter in the Great Lakes.
  • Impact Subcriterion: In addition, the species has been known to impact other systems which it has invaded or is assessed as likely to impact the Great Lakes system.
  • Alternatively, the species has been officially listed as a potential invasive species of concern by federal, state or provincial authorities with jurisdiction in the Great Lakes basin.
  • Alternatively, the species was previously established (evidence of overwintering and reproduction below the ordinary high water mark) but the population subsequently failed.
Three species included in the GLANSIS Watchlist (Cherax quadricarinatus, Monochoria hastata, and Salvinia minima) were excluded from the current analysis as unlikely to survive to establish in either current or 2050 scenarios. This analysis included all other species (n = 94) on the GLANSIS watchlist. Collectively, the GLANSIS bibliographies for watchlist species include 5622 original English-language sources at the time of analysis [bibliographies are publicly available through GLANSIS profiles for each species at https://www.glerl.noaa.gov/glansis/ (accessed on 20 May 2025)].
While all sections of GLANSIS risk assessments and profiles were used as sources for this secondary analysis, Section B10 of each individual species assessment included information previously collated to answer the question ‘How likely is this species to adapt to or benefit from the predicted effects of climate change on the Great Lakes freshwater ecosystems (e.g., warmer water temperatures, shorter duration of ice cover, altered streamflow patterns, increased salinization)?’ which yielded particularly relevant information for examination of future scenarios.
Current and projected temperatures for the Great Lakes region used in our analysis were previously compiled in part by the Great Lakes Integrated Sciences Assessment (GLISA) program. GLISA datasets include a large number of environmental and socioeconomic factors included in climate change, but we chose to limit our study to just a handful of baseline thermal parameters (Table 1). These thermal parameters are the best available direct projections of temperature included in the basin-wide datasets and best map directly to thermal tolerance information available for the majority of GLANSIS Watchlist species.
Maximum average water temperature for each lake projected for 2050 is based on averaging the Intergovernmental Panel on Climate Change (IPCC) A2 and B2 scenarios for the 2041–2070 period [38]; minimum and maximum average air temperatures projected for 2050 are based on the IPCC A1fi scenario [39]. All other projections for the mid-century rely on the IPCC A2 or Representative Concentration Pathway (RCP) 8.5 scenarios, dependent on the scenarios’ state of publication at the time of projection modeling [19,40,41,42]. Due to data limitations, values for maximum average and extreme water temperature are shared between Michigan and Huron. Maximum extreme water temperature for Lakes Michigan and Huron do not take into account that the southern end of Lake Michigan, Green Bay, and Saginaw Bay experience extremes 2–3 degrees higher than the rest of the respective lake [40,43]. Maximum extreme water temperature for Lake Erie does not take into account nearshore shallow areas such as Sandusky Bay, where surface temperatures are expected to be 1–2 °C warmer than listed temperature for primarily offshore areas [38]. The number of days above 10 °C temperatures for Lake Superior is based on open water; inshore temperatures are expected to be more variable [38]. The number of days above 32.2 °C air temperature for Lake Michigan coastal zones does not reflect the Chicago urban area, which currently experiences much more frequent extreme heat days annually (15 days).
Table 1. Current conditions and 2050 thermal projections used as criteria for evaluating potential survival of watchlist species (per Table 2). Temperatures in °C.
Table 1. Current conditions and 2050 thermal projections used as criteria for evaluating potential survival of watchlist species (per Table 2). Temperatures in °C.
ParameterScenarioSuperiorMichiganHuronErieOntarioSources
Maximum Average Water Temperature202515.119.719.723.321.6[38]
205018.621.821.824.824.0[38]
Maximum Extreme Water Temperature202518.122.722.723.324.6[38]
205021.624.824.827.827.0[38,40]
Days above 10 °C Water Temperature202585134134184149[38]
2050131168168217189[38]
Ice Cover (Ice Days)2025189182182168175[44]
2050159165157148161[19,44,45]
Minimum Average Air Temperature2025−16.2−8.4−8.4−5.8−9.7[46]
2050−12.2−4.9−4.9−2.3−6.2[39,46]
Max Average Air Temperature202522.627.227.226.425.2[46]
205025.930.530.529.728.5[39,46]
Days above 32.2 °C
Air Temperature
20252.158.28.27.53.4[46]
205012–3218–5828–4828–5823–43[42]
Frost-free Season (days)2025112–161133–192112–192143–212122–192[47]
2050132–181153–212132–212163–232153–212[42,48]
Species-specific information relating to temperature tolerances of the watchlist species was compiled from the individual assessments and profiles previously published for each of these species in GLANSIS. For each species the tolerance data was compared to the current and projected water temperature parameters to determine likelihood that each lake would support survival of the species in current and projected thermal conditions. Likelihood of survival was scored qualitatively using objective criteria (Table 2).
In order to account for species requiring a habitat which offers a certain duration of the presence of optimal temperatures (e.g., for purposes of successful reproduction), species whose optimal temperature range is greater than 15C include a condition of at least 175 (offshore species) or 150 (nearshore species) predicted days of surface temperatures above 10C for a lake to fulfill the “yes” grade in that category. A “yes” grade in the category of winter conditions also includes species with recorded oxygen/temperature tolerances necessary for overwintering [32]. Similarly, a “probably” grade in the same category can also be assigned if a species’ oxygen or temperature tolerance suggests an ability to overwinter, but requires additionally that no evidence exists that a species would be limited in its survival by the winter conditions of the Great Lakes.
Table 2. Criteria for qualitative assessment of potential survival of watchlist species based on thermal parameters.
Table 2. Criteria for qualitative assessment of potential survival of watchlist species based on thermal parameters.
ParameterYesProbablyPossiblyUnlikelyNo
Temperature MaximumSpecies’ water temperature range falls fully within predicted extreme maximum water temperatures.Species’ water temperature range is not known in full, but mostly falls within predicted average high water temperatures, or the species is known to inhabit colder water below the summer thermocline.Insufficient data, but range indicates a possibility of survival in expected high average water temperatures.Data is limited, but suggests a low tolerance for expected water temperature maximums; species may engage in adaptive behaviors to avoid high-temperature regions.None of the lakes are expected to have cool enough surface temperatures for this species’ survival, and they are unlikely to inhabit colder water below the summer thermocline.
Optimal
Temperature
Species’ optimal temperature range or temperature required for reproduction falls within −6 °C or +2 °C of expected maximum average temperatures.Conflicting information exists on species’ optimal temperature range, but conditions described by at least one set of data are available.A lake meets one of the previous qualifications under the “Yes” condition, but not verifiably both.No lake is likely to consistently meet the species’ optimal temperature conditions, but they may be temporarily present, or exist in small and specific areas of a lake.None of the lakes are reasonably expected to meet the species’ optimal temperature conditions.
Winter
Conditions
The species is known to overwinter in equivalent to or harsher conditions than expected winter conditions.The species adapts behaviorally to winter conditions and/or is known to overwinter under ice cover conditions that are not as extreme as those expected in the lakes. Data may be limited, but does not contraindicate an ability to overwinter, and/or specific habitat conditions are preferred for successful overwintering.Data is limited, but suggests a low tolerance for winter conditions.Data indicates species will not be able to tolerate expected winter conditions.
Air
Temperature Extremes *
The species’ existing range and/or recorded tolerances fully include the expected climatic conditions. The species’ recorded tolerances mostly include the expected climatic conditions such that local variation is likely to provide appropriate habitat.Data may be limited, but does not contraindicate the potential of climatically appropriate available habitat.Data suggests an overall inability to tolerate expected climate conditions in any lake, but species may find habitat in a few specific locations due to variability.The species is definitively unable to tolerate expected extreme air temperature conditions in the region of any lake.
Optimal
Climate *
The species’ optimal air temperature range, thermal conditions required for growth/reproduction, or necessary frost-free season is consistently present within the area/shoreline.The species’ optimal climate conditions are likely to be present within the region The species’ optimal climate conditions have the potential to be present, but are not expected to be consistently present over multiple years.No lake region is likely to consistently meet the species’ optimal climate conditions, but they may be temporarily present in some years, or exist variably in small pockets of the region.No lake region is expected to meet the species’ optimal climate conditions.
* Applies only to species likely to be extensively exposed to open-air conditions due to preferred habitat or life cycle.
For each species and each of the parameter pairs (current and 2050) the change in qualitative assessment was assigned as
  • Increased Risk—Based on an increase in overlap over time between lake conditions and species temperature parameters, temperature effects expected as a result of 2050 climate change will make the Great Lakes more hospitable to this species than previously.
  • Neutral—The species is equally as likely to establish in 2050 climate conditions as it is currently/historically.
  • Decreased Risk—The effects of 2050 climate change will decrease the amount of viable thermal habitat for this species.
  • Insufficient information—Data is insufficient to make a judgment.
Separate from the effects of climate change experienced by an individual species as delineated above, a semi-quantitative threat index was used on an individual lake-level basis to assign species to the lakes with varying degrees of potential habitat in current and expected 2050 conditions:
  • High—An individual lake was identified as consistently containing viable thermal habitat across parameters for a species.
  • Medium—The individual lake was identified as only partially fulfilling a species’ thermal habitat requirements in at least one parameter, or doing so inconsistently.
  • Low—The individual lake fell entirely outside at least one thermal parameter for a species.
Maps were created using ArcGIS® software by Esri (ArcGIS Pro v3.3, Esri, Redlands, CA, USA). To create paired summary maps the Great Lakes shoreline layer (Source: GLAHF) was first transformed from its original North American Datum (NAD) 1983 coordinate system to World Geodetic System (WGS) 1984. The number of species with viable temperature habitat, derived from the analysis, was joined to the shoreline layer’s attribute table. This layer was used to create two separate map visualizations portraying the number of species per lake for both current and 2050 temperature projections. Symbology was adjusted to a yellow-red color ramp representing the number of species. Both final map layouts were projected using the WGS 1984 Web Mercator coordinate system.

3. Results

3.1. Impact of Lake Warming on the Establishment Risk for Watchlist Species

Ninety-seven species on the current GLANSIS Watchlist were assessed for survival in current and projected thermal regimes. Three of these species (Cherax quadricarinatus, Monochoria hastata, and Salvinia minima) were found to be unlikely to survive in either current or projected temperature conditions and eliminated from further analyses. The remaining 94 species represent a diverse taxonomic assemblage including crustaceans (30%), fish (27%), plants (19%) and other (24%) species that are not native to the Great Lakes basin (Table 3). Insufficient thermal tolerance information was available to assess likelihood of survival for 15 species (16%). Of those for which sufficient information was available, 43 species (54%) were found to pose an increased risk of surviving under projected warmer conditions, while only 6 species (6%) were found to have a decreased risk of survival. Thirty-one species (39%) were neutral to the projected thermal changes (likelihood of survival neither increasing nor decreasing with projected temperature).
Taxonomic groups differ in their thermal tolerances and as a result differ in the change in likelihood of survival under warmer temperature conditions (Figure 2). All non-native herps included in the current watchlist (n = 5) benefited from the warmer thermal regime. Almost 75% of current watchlist plants (n = 18) also benefited from warmer temperatures and extended growing seasons.
Table 3. Impact of projected thermal changes on the establishment risk for watchlist species. Current Establishment Risk from GLANSIS Assessments [31,32,33,34,35,36]. ‘Failed’ indicates that a population was previously introduced to the Great Lakes with evidence of overwintering and reproduction prior to failure of the population. Establishment risk was otherwise based on a semi-quantitative assessment described in [32]. Risk change in the 2050 scenarios is relative to this baseline.
Table 3. Impact of projected thermal changes on the establishment risk for watchlist species. Current Establishment Risk from GLANSIS Assessments [31,32,33,34,35,36]. ‘Failed’ indicates that a population was previously introduced to the Great Lakes with evidence of overwintering and reproduction prior to failure of the population. Establishment risk was otherwise based on a semi-quantitative assessment described in [32]. Risk change in the 2050 scenarios is relative to this baseline.
Taxonomic GroupWatchlist SpeciesCurrent Establishment
Risk
Increased RiskNeutral
Risk
Decreased RiskInsufficient Information
AlgaeChaetoceros muelleriFailedx
(n = 9)Hymenomonas roseolaFailedx
Pleurosira laevisFailedx
Prymnesium parvumModeratex
Sphacelaria fluviatilisFailed x
Sphacelaria lacustrisFailed x
Thalassiosira bramaputraeFailed x
Ulva intestinalisFailed x
Ulva proliferaFailed x
PlantsAlternanthera philoxeroidesModeratex
(n = 18)Arundo donaxHighx
Crassula helmsiiModeratex
Egeria densaModerate x
Egeria najasModeratex
Eichhornia crassipesModeratex
Hottonia palustrisModerate x
Hygrophila polyspermaModeratex
Impatiens balfouriiModeratex
Ludwigia grandifloraHighx
Lysimachia punctataModerate x
Myriophyllum aquaticumModeratex
Lagarosiphon majorModeratex
Nelumbo nuciferaHighx
Oenanthe javanicaModeratex
Pistia stratiotesModeratex
Sparganium erectumModerate x
Typha laxmanniiModerate x
HerpsKinosternon subrubrumModeratex
(n = 5)Pseudemys concinnaModeratex
Macrochelys temminckiiLowx
Trachemys scripta scriptaModeratex
Xenopus laevisHighx
FishesAlburnus alburnusHighx
(n = 25)Alosa chrysochlorisModerate x
Babka gymnotrachelusHigh x
Carassius carassiusModeratex
Channa argusModeratex
Clupeonella cultriventrisModerate x
Cyprinella lutrensisHigh x
Cyprinella whippleiModeratex
Hypophthalmichthys molitrixModerate x
Hypophthalmichthys nobilisModeratex
Ictalurus furcatusModerate x
Knipowitschia caucasicaModerate x
Lepomis auritusModeratex
Leuciscus idusModerate x
Leuciscus leuciscusModeratex
Mylopharyngodon piceusModerate x
Neogobius fluviatilisHigh x
Osmerus eperlanusModerate x
Perca fluviatilisHighx
Percottus gleniiHigh x
Phoxinus phoxinusModerate x
Rutilus rutiliusModerate x
Sander luciopercaModeratex
Syngnathus abasterModerate x
Tinca tincaModeratex
CrustaceansApocorophium lacustreModerate x
(n = 28)Astacus astacusLow x
Calanipeda aquaedulcisModerate x
Chelicorophium curvispinumModerate x
Cherax destructorModeratex
Cornigerius maeoticusModerate x
Cyclops kolensisModerate x
Daphnia cristataHigh x
Dikerogammarus haemobaphesHighx
Dikerogammarus villosusHigh x
Echinogammarus warpachowskyiModerate x
Faxonius limosusModerate x
Heterocope appendiculataModerate x
Heterocope caspiaModerate x
Limnomysis benedeniHigh x
Obesogammarus crassusHigh x
Obesogammarus obesusHigh x
Pacifastacus leniusculusHigh x
Paraleptastacus spinicaudusModerate x
Paraleptastacus wilsoniModerate x
Paramysis intermediaModeratex
Paramysis lacustrisModeratex
Pontogammarus robustoidesModeratex
Procambarus virginalisHighx
Pseudorasbora parvaModeratex
Rhithropanopaeus harrisiiHigh x
Silurus glanisHighx
Sinelobus stanfordiModeratex
Other—Annelid (n = 1)Hypania invalidaModerate x
Other—Bryozoan (n = 1)Fredericella sultanaModerate x
Other—MollusksHypanis colorataModeratex
(n = 3)Limnoperna fortuneiModeratex
Lithoglyphus naticoidesModerate x
Other—Platyhelminthes
(n = 1)
Leyogonimus polyoonModerate x
Other—RotifersBrachionus leydigiiModerate x
(n = 3)Filinia cornutaModerate x
Filinia passaModerate x
Figure 2. Taxa posing a greater risk under projected thermal changes. Horizontal line indicates the overall percentage of watchlist species expected to benefit from climate change.
Figure 2. Taxa posing a greater risk under projected thermal changes. Horizontal line indicates the overall percentage of watchlist species expected to benefit from climate change.
Diversity 17 00861 g002

3.2. Geographic Differences in Risk

Projected temperature changes differ across the Great Lakes, with northern Lake Superior having slightly greater projected changes than southern reaches. Lake Superior’s projected vulnerability (change in number of species posing a threat) increased by 17%, Lake Huron by 8%, Lake Michigan by 5%, Lake Erie by 2% and Lake Ontario by 1% (Figure 3). The projected thermal changes in northern Great Lakes cross the threshold of thermal tolerance for many species; current conditions that create a thermal barrier to the survival of these species in Lake Superior and Lake Huron disappear in the projected thermal conditions. This shift is not equally offset by the potential for ‘too warm’ conditions to create a barrier for survival of these species in the southern portions of the Lakes.
Figure 3. Paired maps depicting the number of species assessed as posing a medium or high establishment threat to each lake under current and projected thermal regimes.
Figure 3. Paired maps depicting the number of species assessed as posing a medium or high establishment threat to each lake under current and projected thermal regimes.
Diversity 17 00861 g003

4. Discussion

Understanding potential changes to the risk posed by invasive species is critical to the management of the Great Lakes. Binational, federal, state, tribal and local authorities invest significant resources in surveillance for potential invasives and in rapid response to discoveries. To remain efficient, surveillance programs need to adapt and invest resources to pathways, taxa and geographic locations that pose the highest risk. Forty-six percent of the species analyzed here were found to pose an increased risk of establishing under 2050 projected thermal conditions, while only seven percent were found to pose a decreased risk. While the sample size was small, the potentially invasive herpetofauna (amphibians and turtles) were universally found to pose an increased risk of establishment under warmer scenarios, and nearly 75% of the potentially invasive aquatic plants were likewise found to pose an increased risk for survival. Geographically, the northern portions of the Great Lakes, especially Lakes Superior and Huron, are projected to become more vulnerable to potential invasion by new species.
Hellman et al. [13] outlines five categories of consequences of climate change for invasive species: (1) altered transport of invasive species, (2) altered climatic constraints on invasive species, (3) altered distributions of existing invasive species, (4) altered impact of existing invasive species, and (5) altered effectiveness of management strategies. This study limited its scope to potential direct impacts of changes to the thermal regime on survival/establishment of the watchlist species—firmly within Hellman’s second category. Indirect impacts of climate change (such as elimination of native competitors and changes to habitat—e.g., acidification, stratification, water levels, currents, storm frequency) and potential simultaneous system changes which may not be related to climate change (e.g., human population shifts, changes in vectors, land use changes) were not considered. Such additional future scenarios may either aggravate or counterbalance the direct effects summarized here. Buckley et al. [28] conducted a broader assessment of vulnerability of the Great Lakes (including Canadian inland lakes of the basin) to invasive species (including both already established species and introduction, which we did not consider) in response to the combined effects of climate and human population change; their results reflect ours in that aquatic plants show an increased risk of invasion, with northern areas more vulnerable to invasion, while planktonic invertebrates exhibit decreased risk in the Great Lakes. They subdivided their assessment of fishes into aquarium fishes, baitfish, and warmwater fishes while excluding coldwater fishes, which may provide a more nuanced explanation for our mixed results (only 40% of the watchlist fishes examined here showed increased potential for establishment under warmer conditions).
The scope of this study was limited to the pre-existing GLANSIS watchlist, a subset of potential invaders for which exhaustive literature reviews had already been conducted. While generated using consistent methods and intended as a representative sample, this watchlist is not exhaustive of all potential invaders to the Great Lakes—a recent horizon scan conducted by a co-author on this paper [36] has identified an additional 667 species which, based on rapid assessment, may meet listing criteria. Campbell et al. [26] looked at the history of failed fish introductions to the Laurentian Great Lakes and identified 7 fish species from that set (n = 34) that were likely to have an increased climate match and increased establishment success under future scenarios. Unfortunately, none of these seven are included in the current GLANSIS watchlist, so were not included in this analysis (four of the seven are in the set identified in our horizon scan, Gambusia affinis is reported as already established in Wisconsin waters of Lake Michigan, Morone mississippiensis is native to southern Lake Michigan tributaries, and Pycocentrus natteri had been missed in our horizon scan). Additional examinations of potential biases in the GLANSIS watchlist and in the literature consulted for these species are available as part of a larger gap analysis conducted on GLANSIS [49].
The scope of this study was similarly limited to the projected effects of climate change on the physical thermal conditions of the Great Lakes. As such, other projected effects of climate change with the potential to impact the establishment of aquatic invasive species (e.g., changes to existing Great Lakes aquatic species populations [20], or runoff-based alterations to nutrient loads [50]) were not considered in this analysis. At this time, there is no published research focusing on the relationship between non-thermal climate change effects and the suitability of the Great Lakes for invasion.
Very few peer-reviewed studies have included a detailed examination of the influence of climate change on species invasions in the Great Lakes, despite a wealth of readily available information on the ecology of current and potential invasive species and detailed climate projection models for the region. However, this information is likely to be critical for informing efficient use of limited surveillance and management resources. This current analysis is low-resolution and limited in scope, but we believe it provides insights to guide future research. In the future we hope to work to similarly address Hellman’s third category of climate consequences to the Great Lakes (altered distributions of existing invasive species) using a more refined geographic framework and existing GLANSIS information. Data and metrics available through GLANSIS impact assessments may also be useful as a baseline in predicting Hellman’s first (altered transport of invasive species), fourth (altered impact of existing invasive species), and fifth (altered effectiveness of management strategies) categories, but these would require more extensive modeling and social-science projections not currently available through GLANSIS.

Author Contributions

Conceptualization: R.S.; Methodology, Investigation and Formal Analysis: E.H.; Data Visualization: E.H. and C.S.; Writing: R.S. and E.H.; Project Administration: R.S. All authors have read and agreed to the published version of the manuscript.

Funding

Funding for this project was provided by the COOPERATIVE INSTITUTE FOR GREAT LAKES RESEARCH (CIGLR) through the National Oceanic and Atmospheric Administration (NOAA) Cooperative Agreement with the University of Michigan (NA22OAR4320150). This is CIGLR contribution #1271. Michigan Sea Grant contributions to this research were funded under awards NA24OARX417C0157-T3-01S001 and -01S005 by the GREAT LAKES RESTORATION INITIATIVE, U.S. ENVIRONMENTAL PROTECTION AGENCY, via the NATIONAL OCEANIC AND ATMOSPHERIC ADMINISTRATION, U.S. DEPARTMENT OF COMMERCE, through the Regents of the University of Michigan. The statements, findings, conclusions, and recommendations are those of the author(s) and do not necessarily reflect the views of the National Oceanic and Atmospheric Administration, the Department of Commerce, or the Regents of the University of Michigan.

Data Availability Statement

All raw data for species characteristics and environmental limits along with the full bibliographies can be found at GLANSIS (www.glerl.noaa.gov/glansis) (accessed on 20 May 2025)—either in the individual species profiles or the risk assessments.

Acknowledgments

Ashley Elgin, NOAA Great Lakes Environmental Research Laboratory, served as fellowship co-mentor for Elias Hanson.

Conflicts of Interest

The authors declare no conflicts of interest. The funders had no role in the design of the study; in the collection, analyses, or interpretation of data; in the writing of the manuscript; or in the decision to publish the results.

Abbreviations

The following abbreviations are used in this manuscript:
GLANSISGreat Lakes Aquatic Nonindigenous Species Information System
NOAANational Oceanic and Atmospheric Administration
GLERLGreat Lakes Environmental Research Laboratory
USGSUnited States Geological Survey
USDAUnited States Department of Agriculture
GLAHFGreat Lakes Aquatic Habitat Framework
GLISAGreat Lakes Integrated Sciences and Assessments Center
NADNorth American Datum
NGSNational Geodetic Survey
WGSWorld Geodetic System

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MDPI and ACS Style

Hanson, E.; Shelly, C.; Sturtevant, R. A Secondary Analysis of Invasion Risk in the Context of an Altered Thermal Regime in the Great Lakes. Diversity 2025, 17, 861. https://doi.org/10.3390/d17120861

AMA Style

Hanson E, Shelly C, Sturtevant R. A Secondary Analysis of Invasion Risk in the Context of an Altered Thermal Regime in the Great Lakes. Diversity. 2025; 17(12):861. https://doi.org/10.3390/d17120861

Chicago/Turabian Style

Hanson, Elias, Connor Shelly, and Rochelle Sturtevant. 2025. "A Secondary Analysis of Invasion Risk in the Context of an Altered Thermal Regime in the Great Lakes" Diversity 17, no. 12: 861. https://doi.org/10.3390/d17120861

APA Style

Hanson, E., Shelly, C., & Sturtevant, R. (2025). A Secondary Analysis of Invasion Risk in the Context of an Altered Thermal Regime in the Great Lakes. Diversity, 17(12), 861. https://doi.org/10.3390/d17120861

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