Despite decades of awareness about the biodiversity crisis, it remains a wicked problem. Besides preservation and restoration strategies, one approach has focused on increasing public concern about biodiversity issues by emphasizing opportunities for people to experience natural environments. In this article, we endeavor to complicate the understanding of these experiences of nature (EoN). Because EoN are embedded in social and cultural contexts, transformative or new EoN are emerging in combination with societal changes in work, home, and technology. Policies that acknowledge and accept a diversity of culturally situated EoN, including negative EoN, could help people reconnect with the complexity and dynamics of biodiversity. A new conceptualization of EoN that encompasses diverse experiences and reflects the sociocultural context could help to stimulate a broader transformation in the relationship between society and nature, one that better integrates the two spheres. Such a transformation is necessary to more effectively address the biodiversity crisis.

[1] A decadal resolution time series of sea surface temperature (SST) spanning the last two millennia is reconstructed by combining a proxy record from a new sediment sequence with previously published data from core MD99-2275, north of Iceland. The alkenone based SST reconstruction is validated with historic observational data and compared to a new similar temporal resolution reconstruction obtained from sediment core RAPiD21-3K, in the subpolar North Atlantic. The two SST paleorecords show consistent multidecadal scale coolings throughout the interval and similar expressions during the contrasted climatic periods 'colloquially known' as the Medieval Climatic Anomaly (MCA) and Little Ice Age (LIA). In order to further understand the temporal and spatial SST variations and investigate the influence of natural forcings on the observed SST changes during the last millennium, we compare our time series to simulations using the Institut Pierre-Simon Laplace IPSLCM4-v2 climate model. This comparison highlights the potential importance of volcanism as a natural forcing driving coherent abrupt cooling events captured in the subpolar North Atlantic records.