Ecological boundaries must be incorporated in the post-COP30 climate regime
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A Nature Portfolio journal
https://doi.org/10.1038/s43247-026-03337-x
Ecological boundaries must be incorporated
in the post-COP30 climate regime
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Qinglong Shao
The 2025 United Nations Climate Change
Conference COP30, was held in Belém, Brazil at the
mouth of the Amazon River. The location brought
global attention to the ecological systems that
underlie climate stability: as one of the world’s most
important biophysical regulators, the Amazon basin
exemplifies how forests, hydrological cycles,
biodiversity, and Indigenous stewardship
collectively shape regional and global climate
dynamics. Scientific briefings at the conference
emphasized the accelerating pressures on these
systems, from deforestation and ecosystem
conversion to freshwater decline and coastal
degradation, as well as their implications for climate
outcomes, consistent with growing recognition
across climate policy processes.
At COP30, Parties and observers emphasized forest protection, ecosystem
restoration, and nature-based solutions as integral to climate mitigation and
adaptation discussions1,2. A central theme of these discussions was the
framing of climate change and biodiversity loss—as a core dimension of
ecosystem degradation—as mutually reinforcing crises, and the recognition
that climate and biodiversity policy frameworks have long evolved in parallel but largely in isolation. Within these discussions, leading scientists
highlighted that climate change and biodiversity loss arise from deeper
disruptions in human–Earth-system relationships, and cautioned that
ongoing ecosystem degradation can further undermine the feasibility of
both mitigation and adaptation, making biodiversity considerations central
rather than peripheral to climate policy (Nathalie Seddon, University of
Oxford)2. This emphasis was reinforced by initiatives advanced by the
Brazilian presidency, such as the Tropical Forests Forever Facility, aimed at
mobilizing long-term finance for tropical forest conservation within broader
climate action efforts3. Together, these discussions reflect a growing
recognition within climate governance that pressures on ecosystems are
closely linked to climate outcomes. This policy recognition aligns with
Earth-system assessments showing that land-use change, deforestation, and
ecosystem degradation can amplify climate change through carbon-cycle
and hydrological feedbacks4.
Nevertheless, despite the insight that ecosystem degradation directly
and indirectly affects the climate, the formal United Nations Framework
Convention on Climate Change (UNFCCC) negotiations were predominantly centered on emissions pathways, fossil-fuel transition, and
Communications Earth & Environment | (2026)7:263
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climate finance architecture5. These priorities directly reflect the structure of
the Paris Agreement, which was designed around mitigation and adaptation. But they also reveal an emerging challenge. Global climate governance
has yet to fully establish and integrate ecological boundaries to the resilience
and functioning of the climate system6,7, there are limits to the disturbances
that biophysical ecosystem processes can endure—and still stabilise the
Earth’s climate.
Here we argue that climate governance requires the explicit inclusion of
nature-based boundaries—alongside, rather than in place of, emissions
metrics—to improve the coherence, predictability, and resilience of the
climate regime. As countries prepare for the next round of Nationally
Determined Contributions (NDC 3.0) and the second Global Stocktake,
now is the time to incorporate ecological indicators in these frameworks.
Ecological trends and climate risk. Ecological destabilization can erode
the benefits of emissions-focused climate strategies. Specifically, ecosystems regulate water and carbon cycles that directly affect the climate. For
example, declining resilience in tropical forests reduces moisture recycling
and carbon-sink stability8; ongoing biodiversity loss undermines the
functional redundancy in ecosystems that is needed to buffer climatic
extremes9; and degradation of blue-carbon systems—such as mangroves—
releases long-stored carbon while also weakening natural coastal defenses
that buffer shorelines against sea-level rise and storm surges, thereby
amplifying a key climate impact10. In addition, mitigation strategies—such
as large-scale bioenergy production and afforestation—can affect ecosystems by putting pressure onto freshwater, nutrient cycles, and habitats11.
Together, these dynamics suggest that mitigation efforts yield smaller and
less reliable climate benefits when ecological boundaries are under stress.
Forest and land-system change. Tropical forest ecosystems such as the
Amazon constitute a critical ecological boundary for climate stability,
where forest cover, hydrological processes, and atmospheric circulation
are tightly coupled (see Fig. 1)12. For the Amazon basins, recent studies
highlighted growing tipping-point risks associated with continued
declines in forest cover and the weakening of land–atmosphere and
hydrological feedbacks that regulate regional rainfall13,14. Noteworthy, a
side event at COP30 entitled “Global Tipping Points reports: solutions for
the Amazon” illustrated that the interactions between deforestation,
climate warming, and fire are pushing large parts of the Amazon closer to
critical ecological thresholds. Speakers underscored that crossing such
thresholds could trigger irreversible changes in moisture recycling,
drought frequency, and regional climate stability, reinforcing concerns
that ecosystem degradation in the Amazon is a key driver of systemic
climate risk15.
Biodiversity decline and ecosystem resilience. Biodiversity underpins functional redundancy, nutrient cycling, and ecosystem stability.
Losses in pollinator diversity, soil organisms, and keystone species can
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Fig. 1 | Coastal forest ecosystems as an ecological boundary for climate resilience.
Coastal forested wetlands exemplify ecological boundaries where land, water, and
biological processes interact to regulate carbon storage and protection against climate extremes. Degradation of such boundary systems can undermine ecosystem
stability and amplify climate-related risks. Photo by Jiankun He.
reduce adaptive capacity, increasing the vulnerability of ecosystems to
heatwaves, droughts, and disease outbreaks16. These ecological degradations also diminish the ability of natural systems to buffer extreme
climatic events.
Blue-carbon systems and coastal protection. Mangroves, seagrasses,
and tidal wetlands are among the planet’s most efficient long-term carbon stores. They also reduce flooding and prevent shoreline erosion;
when degraded, these protective functions are lost, increasing vulnerability to sea-level rise17. In addition, pressures from aquaculture, land
reclamation, and coastal development cont (...truncated)