Cave Discovery Reveals Today’s Desert Climates Were Recently Far Warmer, Wetter, Teeming With Life

From the NoTricksZone

By Kenneth Richard

Fuerteventura, one of the eight major Canary Islands, was not the “desert in the ocean” it is today throughout the Early to Middle Holocene.

Scientists (Sánchez-Marco et al., 2026) have recovered the remains of several bird species known to reside at the edges of bodies of water (e.g., lagoons, lakes, rivers) with riparian vegetation and dense forests from a cave in Fuerteventura, the most arid of the Canary Islands. The bones date to ~9000 to 5000 years ago.

This discovery “unexpectedly” reveals the Holocene climate was much warmer (as much as “3 to 7°C”) than present. It was also “much wetter than it is today” a few thousand years ago, and thus regions that are today arid and largely uninhabitable were recently able to host to far more plant and animal species diversity.

The cooler Fuerteventura environment is today covered in sand dunes and classified as an arid desert, as it receives only 100-150 mm of rain annually. The island no longer supports water fowl habitat or any other species dependent on large annual rainfall totals.

“Recent ice core analysis from northern Greenland reveals that the highest Holocene temperatures would occur between 10 and 7 ka BP, 3 to 7 °C warmer than today. This suggests that the animals studied here died in warmer conditions than those prevailing today.”

“It seems likely that there was a lagoon or pond near the cave, around which large areas of riparian vegetation developed. Likewise, wooded areas with undergrowth, where there were even wrynecks, were probably also in the vicinity of the cave. The ornithological record from Cueva del Llano suggests that in the early stages of the Holocene, the dominant climate in the Canary Islands was much wetter than it is today. In Fuerteventura, there were bodies of water with riparian vegetation and more or less dense forest areas with shrubby undergrowth. Higher global temperatures than the present ones may have led to changes in the annual displacements of the Azores High and promoted a more intense rainfall regime, which fostered the maintenance of more diverse habitats and, consequently, a significantly more diverse avian fauna than today. The birds linked to these habitats likely disappeared with climate changes, which led to notably more xeric conditions.”

Canary-Islands-bird-species-remains-suggest-Holocene-was-3-7C-warmer-and-much-wetter-than-today-Sanchez-Marco-2026

Image Source: Sánchez-Marco et al., 2026

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Neil Pryke
April 13, 2026 10:15 pm

Fuerteventura was “trendy” in the 80s and 90s…the only fossils were the drinks-party types bandying the name about…

April 13, 2026 10:33 pm

Maybe the AMOC was “collapsed” back then? 😉

Stephen Wilde
April 13, 2026 11:23 pm

The main pressure cells such as the Azores high move around as necessary to maintain a global temperature determined only by solar input, atmospheric mass and the downward force of gravity.
Such movement adjusts the rate at which energy is lost to space so as to balance the upward pressure gradient within the atmosphere with the downward force of gravity.
That principle applies to every planet with any sort of atmosphere.
The thermal effects of other factors such as radiative gases are similarly neutralised by such movements within the convective overturning of any atmosphere.
Without such a balancing process an atmosphere is lost to space or solidifies on the ground.
Recent climate science has been a complete disaster.