Non-pollen palynomorphs (NPPs) form a large group of biological objects found in
palynological slides besides pollen grains. This includes various remains of algae and fungi …

Only a few studies have related modern non-pollen palynomorphs to environmental
variables, limiting the development of non-pollen palynomorphs training sets. Here, we …

The middle Miocene Climate Optimum (MMCO) was the warmest interval of the last 23
million years and is one of the best analogs for proposed future climate change scenarios …

Few latest Cretaceous fossil floras are known for South America, and in particular for the
Austral-Magallanes Basin. Recent studies carried out in the Chorrillo Formation …

Nine non-pollen palynomorph (NPP) groups occur in Quaternary marine and brackish-water
sediments; these groups represent various planktonic or micro-to macrobenthic organisms …

Human‐induced activities around Lake Lilaste in the central Latvian sandy coastal area
have been reconstructed over a 1300‐year period. We use a combination of well …

Madagascar houses one of the Earth's biologically richest, but also one of most endangered,
terrestrial ecoregions. Although it is obvious that humans substantially altered the natural …

Fires are natural phenomena that impact human behaviors, vegetation, and landscape
functions. However, the long-term history of fire, especially in the permafrost marginal zone …

Insect faunas from the latest Cretaceous are poorly known worldwide. Particularly, in the
Southern Hemisphere, there is a gap regarding insect assemblages in the Campanian …

Identification and naming of fossil and subfossil organisms are not easy tasks. We are in the
midst of a paradigm shift in how NPP taxa are named, driven in large part by (1) molecular …