This study explores how climate-driven changes in water balance affected an ancient lake during the Jurassic in Patagonia, and influenced how plant and algal material were deposited and preserved. By combining field observations with palynological analysis, we identified shifts between wetter and drier periods. These shifts controlled lake size, water conditions, and the type and amount of organic matter preserved, improving our understanding of how ancient lake systems record environmental change.

The paper describes the foraminifera of the Eocene in the area of the Hampshire Basin and the English Channel. Hyperthermal events (Early Eocene Climatic Optimum (EECO)) Late Lutetian Thermal Event (LLTE), and Middle Eocene Climatic Optimum (MECO)) are discussed and set in the context of global climate change in the Paleogene.

Oligocene fossils were retrieved from a Miocene deposit. Authors stated that their age should expand into the Miocene accordingly. Miocene age was not directly retrieved from the studied deposits but from a nearby outcrop not clearly connected to the studied succession. We argue that transportation events might have simply reworked Oligocene fossils into the Miocene material, as commonly occurs in ramp environments.

The Maastrichtian–Danian record at Cerro Azul (Argentina) shows shifts in planktic foraminiferal assemblages and sea surface temperatures (SSTs) (TEX^H₈₆) tied to the K–Pg (Cretaceous–Paleogene) extinction. Guembelitriid dominance and high-latitude affinity define the early Danian, with Antarcticella pauciloculata present. At 45 cm above the boundary, tropical species appear with a ~1.5 °C SST rise, signalling initial post-extinction climatic recovery.

The Northwest European Shelf plays a key role in the global carbon cycle. To assess its past role, we want to reconstruct primary productivity using microfossils. By comparing surface sediment assemblages with sediment properties and modern environmental conditions, we found a good microfossil-based indicator for primary productivity. This indicator will be useful to reconstruct productivity in the past Northwest European Shelf.

Well-preserved fossils of Schizopholis were found in the Tsinghsutung Formation of Cambrian Series 2, Stage 4 in Songtao County, Guizhou Province by etching limestones with 3–5% acetic acid. This is the first systematic description of S. yorkensis from South China, and we extend its palaeobiogeographical distribution. Palaeobiogeographical analysis indicates that Schizopholis was predominantly distributed in low-latitude regions and reached its highest abundance/diversity level during the Cambrian Age 4.

Tiny fossils aged 40 x 10⁶ years from an Italian rock section show that the ancient sea's environment was mostly stable. A global warming event caused wetter periods and river runoff into this sea. The study also provides fossil photos and introduces new types, important for future research.

Using the FORCIS database, we mapped the distribution of planktonic goraminifera that record past ocean conditions. Our study reveals that these species mostly inhabit the upper ocean and thrive in waters ranging from −2 °C to over 31 °C. Their range is shifting, with species once limited to warm regions now appearing in cooler areas and smaller species increasing in number. This work refines our view of their biogeography and how climate change is reshaping ocean life.

The Eocene–Oligocene transition was a pivotal interval in Earth's geological history, marked by cooling and Antarctic glaciation. Our research explores how Southern Ocean diatoms responded to these changes. By analyzing records from multiple sites, we revealed previously unrecognized diatom diversity, and identified distinct patterns in diversity and extinction. These findings deepen our understanding of the interplay between climatic perturbations and the biosphere.

Toweius was among the most widespread and important calcareous nannoplankton groups in the oceans 53 million years ago, playing a key role in the evolutionary transition to another prominent group during the Cenozoic (Reticulofenestra). Using detailed biometric measurements with high-resolution imaging, we describe a distinctive, smaller morphotype of Toweius. Our results indicate that this form evolved gradually through speciation, shedding light on the complex evolutionary dynamics of Toweius.

We developed a new global database of microscopic fossil algae, known as calcareous nannoplankton, from Cretaceous ocean sediments to improve the understanding of ancient oceans and climate change. By integrating data from numerous published studies and standardising species names and ages, we created the Uneptune database with about 175 000 fossil records. Hosted on the Nannotax website, it provides visualisation tools that help scientists explore global marine ecosystems during the Cretaceous.