Biodiversity & Ecosystems Crisis Tracking 2026

The Cao-vit gibbon (*Nomascus nasutus*) remains one of the world’s rarest apes and is still classified as Critically Endangered. The most recent population estimate available in the gathered sources is 74 individuals in 11 family groups, based on 2023 vocal fingerprinting and acoustic monitoring research; conservation groups emphasize this is a more accurate census than earlier counts, not evidence of a recent collapse. Recent conservation reporting indicates the species may be stable or slowly increasing, with Fauna & Flora stating the population has doubled over 20 years and that recent surveys revised the count to 74 individuals; related reporting in 2024 also noted patrol-based observations of a troop with infants in the Cao Bằng border forests. The species is restricted to a single transboundary karst forest on the Vietnam-China border, with nine groups in Vietnam and the rest shared or occurring across the border in China, leaving it highly vulnerable to disturbance, disease, and inbreeding.

The Great Barrier Reef experienced mass coral bleaching in 2024 and again in 2025, making this the second consecutive bleaching sequence on record after 2016–2017. AIMS states that the 2024 event was the reef’s fifth mass bleaching since 2016 and part of the fourth global coral bleaching event, which NOAA/ICRI declared in April 2024 after beginning in 2023. AIMS’ 2024/25 condition summary says the 2024 event had the largest spatial footprint ever recorded on the GBR, with high to extreme bleaching across all three reef regions. In 2025, the reef experienced its sixth mass bleaching since 2016; AIMS reported 281 reefs were surveyed across the Torres Strait, the northern GBR, and parts of the central region, and that regional coral-cover declines in 2025 ranged from 14% to 30% compared with 2024, with some reefs losing up to 70.8% of coral cover. NOAA’s global update says bleaching-level heat stress from 1 January 2023 to 30 September 2025 affected about 84.4% of the world’s coral reef area and that mass bleaching has been documented in at least 83 countries and territories.

Global biodiversity loss remains a major and worsening environmental crisis, driven by habitat loss and degradation, land-use change, overexploitation, invasive alien species, pollution, and climate change. The World Health Organization says invasive alien species contribute to 60% of species extinctions and cause about US$423 billion in global economic damage each year, while biodiversity loss overall is estimated to cost the global economy about US$10 trillion annually. Recent evidence continues to show severe ecological decline. WWF’s Living Planet Report 2024 found that monitored wildlife populations declined by an average of 73% since 1970, including an 83% decline in freshwater populations. The European Central Bank also notes that biodiversity loss is highly non-linear and can create large knock-on economic risks, including disruption to ecosystem services such as water filtration, flood protection, pollination, and climate regulation. Policy response remains centered on the Kunming-Montreal Global Biodiversity Framework, but implementation gaps persist. The main affected regions include tropical forests and biodiversity hotspots in Latin America, Africa, and Asia-Pacific, as well as freshwater, wetland, and marine systems worldwide. High-income consumption patterns also drive biodiversity pressure through trade-linked deforestation and ecosystem conversion.

Ocean dead zones are low-oxygen coastal and marine areas that can no longer support most marine life. The latest sources confirm that the main human-driven causes remain nutrient pollution from agricultural runoff, sewage, and industrial waste, which fuels algal blooms; when the algae die, decomposition consumes oxygen. NOAA and Woods Hole Oceanographic Institution both state that warming waters worsen the problem because warmer water holds less dissolved oxygen and stronger stratification reduces vertical mixing and oxygen replenishment. The problem is global and persistent. NOAA describes nutrient pollution as the primary human cause of dead zones, and a widely cited synthesis reported more than 400 dead zones worldwide and a spread that has accelerated since the 1960s. The Baltic Sea remains one of the largest and most persistent hotspots because its semi-enclosed geography limits water exchange, while the Gulf of Mexico continues to experience large seasonal hypoxia linked to Mississippi River nutrient runoff; NOAA’s 2026 forecast was 5,574 square miles, above the long-term average of 5,244 square miles. The issue affects fisheries, biodiversity, and coastal economies, and the scale of human dependence on ocean resources remains very large, but a precise global population directly exposed to dead zones is not available in the sources reviewed.

Indonesia’s coral reefs remain under severe pressure from marine heat stress and bleaching, alongside long-standing local threats such as destructive fishing, pollution, sedimentation, and coastal development. Recent scientific and reporting sources continue to describe widespread reef degradation in Indonesia and across the wider Coral Triangle, with elevated sea temperatures driving mass bleaching and reducing coral cover, fish habitat, and ecosystem services. The crisis is especially important because Indonesia sits at the center of global marine biodiversity, and reef loss can reduce fish nursery habitat, weaken shoreline protection, and harm tourism and coastal livelihoods. Source material also identifies destructive practices such as blast fishing and cyanide fishing, as well as land-based runoff and coastal construction, as persistent drivers of reef decline in Indonesia. However, the provided search results do not include a recent 2025–2026 national reef-cover estimate or a verified countrywide mortality figure, so the latest quantitative severity is not fully established from the available sources.

Madagascar’s food crisis remains concentrated in the Grand South, but the latest IPC snapshot shows a wider June–September 2026 caseload of around 2.12 million people in IPC Phase 3 or above, including more than 183,000 in IPC Phase 4 (Emergency). The most affected areas are in Androy and districts including Tsihombe, Ampanihy Ouest, Bekily, Beloha, Ambovombe-Androy, Antanimora Sud, Amboasary Atsimo, and Toamasina, with Androy alone at about 589,000 people in Phase 3 or above. The crisis is being driven by below-average crop production, depleted household stocks, high prices, livelihood losses, and limited recovery after drought and cyclone shocks. FEWS NET reported that in May 2026 most districts in the Grand South, parts of the Grand Southeast, and cyclone-affected east-coast districts were still in Crisis (IPC Phase 3), while the IPC projection warned that conditions could worsen again to about 3.72 million people in IPC Phase 3 or above during October 2026–February 2027. Recent FEWS NET guidance also notes that seasonal harvests may temporarily improve food access in some areas through September, but drought and cyclone impacts continue to keep needs elevated.

The Mekong Delta continues to lose wetlands, shorelines, and riverbanks because of sediment starvation, sand mining, groundwater extraction, upstream hydropower, and climate stressors such as drought and sea-level rise. IUCN says wetland loss in the Lower Mekong threatens biodiversity, fisheries, water security, infrastructure, and livelihoods for nearly a quarter of a billion people across five countries. In Vietnam’s Mekong Delta, recent and longer-term studies show severe ecological decline. Research has found mangrove area fell from 185,800 hectares in 1973 to 102,160 hectares in 2020, while a review found that less than 5% of the Delta’s natural wetlands remain. Another study links rapid shoreline erosion to reduced sediment supply, large-scale sand mining, and groundwater-driven subsidence, with erosion affecting more than 300 km of shoreline and over 50% of the more than 600 km coast during 2003–2012. Agricultural livelihoods are also under pressure from salinity intrusion and drought. Recent research on Vietnamese Mekong Delta paddy fields reports cumulative paddy loss of 542.98 thousand hectares and net loss of 152.55 thousand hectares from 2000 to 2022, with indirect drivers accounting for 74.86% of losses when urban conversion is excluded. World Bank-linked material cited in the literature reports groundwater extraction-induced subsidence of 1.0–4.7 cm/year in 1991–2016, reinforcing the risk of continued land loss and infrastructure damage.

Brazil’s Amazon deforestation trend is **improving**, with official and independent monitoring showing continued declines into 2026. INPE satellite alerts found **1,325 km²** of clearing from **Aug. 1, 2025 to Jan. 31, 2026**, down from **2,050 km²** a year earlier, and the trailing 12-month total fell to **3,770 km²** from **4,245 km²**; both are the lowest for those periods since 2014. INPE’s PRODES annual system also reported **5,796 km²** of deforestation in the 12 months ending **July 31, 2025**, an **11.08%** decline and the lowest annual total since 2014. The crisis is not over. Reuters and Mongabay report that fire, degradation, cattle ranching, illegal mining, road expansion, and other land-use pressures continue to affect forest stability, even as overall clearing falls. In the first half of 2026, Brazil recorded **1,295 km²** of Amazon deforestation, **38%** below the same period in 2025, and May 2026 was reported as **61.4% lower** than May 2025; however, substantial clearing persisted and the dry season remains a recurring risk.