20The Arctic is experiencing a rapid shift towards warmer regimes, calling for a need to understand 21 levels of biodiversity and ecosystem responses to climate cycles. This study examines marine 22 refugial locations during the Last Glacial Maximum in order to link recolonization pathways to 23 patterns of genetic diversity in Arctic marine forests. We present genetic data for 109 species of 24 seaweed to infer community-level patterns, and hindcast species distributions during the Last 25 Glacial Maximum to further pinpoint likely refugial locations. Sequence data revealed 26 contiguous populations extending from the Bering Sea to the Northwest Atlantic, with high 27 levels of genetic diversity in the East Canadian Arctic. One fifth of the species sampled appeared 28 restricted to Arctic waters. Hindcasted species distributions highlighted refugia in the Bering 29 Sea, Northwest Atlantic, South Greenland, and Europe. We hypothesize that Arctic coastal 30 systems were recolonized from many geographically disparate refugia leading to enriched 31 diversity levels in the East Canadian Arctic, with important contributions stemming from 32 northerly refugia likely centered along Southern Greenland. Moreover, we hypothesize these 33 northerly refugia likely played a key role in promoting polar endemic diversity, as reflected by 34 abundant unique population haplotypes and endemic species in the East Arctic. 35 36 Significance Statement 37 Our work challenges the existing paradigm that marine Arctic ecosystems are depauperate 38 extensions of southerly (temperate) communities established in the wake of recent glaciation, 39 fundamentally changing how these systems should be viewed and interpreted. We forward novel 40 hypotheses regarding the recent history of Arctic marine systems, particularly with regards to 41 endemism being an integral feature of Arctic biomes, and present a firm framework for future 42 evolutionary research in this system typically viewed as "ecologically immature." 43 44 MAIN TEXT 45 46 The Arctic is characterized by a turbulent climatic history and the prospect of further 48 change. Repeated glaciations over the past 2.6 Ma had a lasting impact on biological 49 communities, forcing populations to repeatedly contract and expand with the formation and 50 retreat of ice-sheets (1). Today, warming in the Arctic is significantly exceeding the Northern 51 Hemisphere average, and boreal and temperate regimes are expected to shift northwards as a 52 result (2). A prescient need exists to understand the responses of Arctic marine communities to 53 climate change, a need that will inherently depend on understanding levels of biodiversity, the 54 recent history of Arctic ecosystems, and ultimately the potential for adaptation. 55 56 Marine forests are a model system for providing such insight on Arctic marine 57 communities. Marine forests are structurally complex seascapes created by seaweeds, are 58 ubiquitous worldwide, and provide valuable ecosystem and economic services in the forms of 59 habita...