Abstract

The timing of recurring biological and seasonal environmental events is changing on a global scale relative to temperature and other climate drivers. This study considers the Gulf of Maine ecosystem, a region of high social and ecological importance in the Northwest Atlantic Ocean and synthesizes current knowledge of (a) key seasonal processes, patterns, and events; (b) direct evidence for shifts in timing; (c) implications of phenological responses for linked ecological‐human systems; and (d) potential phenology‐focused adaptation strategies and actions. Twenty studies demonstrated shifts in timing of regional marine organisms and seasonal environmental events. The most common response was earlier timing, observed in spring onset, spring and winter hydrology, zooplankton abundance, occurrence of several larval fishes, and diadromous fish migrations. Later timing was documented for fall onset, reproduction and fledging in Atlantic puffins, spring and fall phytoplankton blooms, and occurrence of additional larval fishes. Changes in event duration generally increased and were detected in zooplankton peak abundance, early life history periods of macro‐invertebrates, and lobster fishery landings. Reduced duration was observed in winter–spring ice‐affected stream flows. Two studies projected phenological changes, both finding diapause duration would decrease in zooplankton under future climate scenarios. Phenological responses were species‐specific and varied depending on the environmental driver, spatial, and temporal scales evaluated. Overall, a wide range of baseline phenology and relevant modeling studies exist, yet surprisingly few document long‐term shifts. Results reveal a need for increased emphasis on phenological shifts in the Gulf of Maine and identify opportunities for future research and consideration of phenological changes in adaptation efforts.

Highlights

  • Changes in phenology, or the seasonal timing of recurring events, have emerged as a primary indicator of species responses to climate change (Parmesan, 2006; Parmesan & Yohe, 2003)

  • Research on marine phenology has a long history in the Gulf of Maine (GoM) region, yet the majority of studies conducted to date have focused primarily on documenting and describing baseline patterns and cycles in seasonal events or developing modeling frameworks to resolve mechanistic relationships of species responses to environmental drivers

  • The results of this synthesis yielded a surprisingly small number of studies (N = 20) showing direct evidence of shifts in timing in biotic and abiotic events. It is possible this is an artifact of under‐reporting non‐significant results, and indicative of stable populations that are adapting in place (Beever et al, 2016; Parmesan, 2007)

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Summary

| INTRODUCTION

The seasonal timing of recurring events, have emerged as a primary indicator of species responses to climate change (Parmesan, 2006; Parmesan & Yohe, 2003). Adult Atlantic herring begin depositing demersal eggs as surface water temperatures decline in late summer through fall (Collette & Klein‐ MacPhee, 2002; Stevenson & Scott, 2005), with larval abundance of fall‐spawned fish peaking in September and October (Figure 4a). Some species such as Atlantic puffins and shearwaters (Ardenna spp., Calonectris spp., Puffinus spp.) are believed to overwinter in nearby habitats of the Gulf of St. Lawrence and Bay of Fundy (Fayet et al, 2017; Powers, Wiley, Allyn, Welch, & Ronconi, 2017), while others, such as roseate (Sterna dougallii), common (S. hirundo), and least terns (Sternula antil‐ larum), migrate as far as South America, and Arctic terns (S. paradi‐ saea) to the Southern Ocean (Egevang et al, 2010; Hays et al, 1997; Nisbet, 1984; Thompson et al, 1997; Veit & Petersen, 1993).

Stratification
Onchidoris muricata
Salmo salar
Findings
| SUMMARY AND CONCLUSIONS
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