Periodic Reporting for period 1 - PLEASE (Impact of climate change on twilight zone fishes during early-stage development)
Reporting period: 2023-03-01 to 2025-08-31
Together, these activities provide a comprehensive understanding of the vulnerability of TLZ communities to climate change, particularly through the effects of ocean warming and acidification on reproduction, larval survival, and species distribution. These findings highlight how alterations in oceanographic conditions can significantly affect the structure and functioning of the TLZ ecosystem, with cascading impacts on global biogeochemical cycles and carbon sequestration.
Moreover, the project evaluated the impact of marine heatwaves on planktonic ecosystems and the abundance of TLZ fish larvae. Using satellite imagery, time series of temperature and chlorophyll-a were reconstructed for the Canary Islands region to detect heatwave events. Two contrasting years were analyzed: 2005 (normal conditions) and 2010 (strong warming and weak phytoplankton bloom). Plankton samples collected near Gran Canaria revealed significantly lower abundances of TLZ fishes belonging to Myctophidae and Gonostomatidae during 2010. These results indicate that marine heatwaves may negatively affect TLZ fish recruitment through reduced food availability and/or altered reproductive success.
In addition, PLEASE developed a global ensemble species distribution model for the TLZ Cyclothone, the most abundant genus of fishes on Earth, to forecast its future distribution under climate change scenarios. Using simulations from the CNRM-ESM2-1 Earth system model, we analyzed ocean variables (temperature, salinity, oxygen, pH, and productivity) from the surface to 2,000 m under pre-industrial, historical, and future SSP2–4.5 and SSP5–8.5 scenarios. Species occurrence data were compiled from field samples and global biodiversity databases, filtered by sampling depth. The model accurately reproduced current habitat suitability and also predicted future range contractions in epipelagic and twilight zones, particularly in the Mediterranean and tropical North Atlantic. These results suggest potential poleward and deeper shifts of Cyclothone populations, with implications for ecosystem resilience and ocean carbon cycling.