Abstract

Old growth is disappearing globally, with implications for biodiversity, forest resilience, and carbon storage; yet uncertainty remains about how much exists, partly because assessments stratify ecosystems differently, sometimes obscuring relevant patterns. This paper compares portrayals of British Columbia’s (BC) old-growth forest stratified in two ways: by biogeoclimatic variant, as per policy, and by relative site productivity. Our analyses confirm provincial government claims that about a quarter of BC’s forests are old growth but find that most of this area has low realized productivity, including subalpine and bog forests, and that less than 1% is highly productive old growth, growing large trees. Within biogeoclimatic variant, nearly half of high-productivity forest landscapes have less than 1% of the expected area of old forest. Low-productivity ecosystems are over-represented in protected forest. We suggest that the experiment of managing old growth solely by biogeoclimatic variant has failed and that current forest policy, in combination with timber harvesting priorities, does not maintain representative ecosystems, counter to the intent of both policy and international conventions. Stratifying old growth by relative productivity within biogeoclimatic variant seems an appropriate method to portray ecosystem representation, potentially increasing the probability of maintaining ecosystem resilience.

Highlights

  • Intact old-growth forest is disappearing globally (FRA 2020), with implications for biodiversity, resilience, and carbon storage (Foley et al 2005; Watson et al 2018)

  • About 13.2 million ha, representing 26% of British Columbia (BC)’s forest, is old growth based on provincial definitions

  • About a quarter of BC’s forests are old growth, less than 1% of BC’s forests (415 000 ha out of 50 million ha) support highproductivity old growth (Table 1; Fig. 1, mostly in patches too small to be visible at this scale); less than 0.1% ($36 000 ha) supports very high productivity old growth

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Summary

Introduction

Intact old-growth forest is disappearing globally (FRA 2020), with implications for biodiversity, resilience, and carbon storage (Foley et al 2005; Watson et al 2018). Old-growth forests are structurally complex natural ecosystems generated by a landscape’s natural disturbance regime (Bunnell 1995; Spies and Franklin 1996; Franklin et al 2002). Structural complexity creates myriad habitats that support diverse communities (e.g., Hamer and Nelson 1995; Winchester and Ring 1996; Radies and Coxson 2004; Cushman et al 2011; Price et al 2017); retaining old growth has long been listed as an important landscapescale component of managing forests for biodiversity (Noss and Cooperrider 1994; Spies and Franklin 1996; Lindenmayer and Franklin 2002). Old-growth forests have been recognized for their substantial carbon stores (Luyssaert et al 2008; Law et al 2018) and resilience to climate change

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