AbstractWe provide a review of micropalaeontological research on Ostracoda from the Middle Pleistocene (MIS 11, Holstein interglacial) hominin site Bilzingsleben in Thuringia in Central Germany from 1963 to the 1990s. Samples from four sections inside and six search pits outside the excavation area were investigated and, in total, 49 ostracod species were identified. The ostracod assemblages of the sections mirror the complex and small‐scale palaeoenvironmental evolution of the site from a seeping‐spring to fluviatile, lacustrine and finally seeping‐spring habitat in which a massive tufa layer formed and prevented erosion of the sediments beneath. Pleistocene index fossils are represented by Ilyocypris quinculminata from search pit 3/sample...
Ostracods as bioindicators are extremely useful for reconstructing palaeoenvironment and palaeoclima...
The Lower Palaeolithic, Middle Pleistocene locality Schöningen has been a focus of archaeological re...
Numerous fossil remains (vertebrates, molluscs and plants) were found in more than twenty sites of t...
Bilzingsleben is internationally known as a palaeontological, palaeoanthropological and archaeologic...
To trace environmental changes of the tectonically active Frasassi area in the northeastern Apennine...
none1noBenthic ostracod analyses performed on a 40 m long core (Core 1) enabled a detailed facies ch...
This thesis deals with the class Ostracoda from the Úpohlavy quarry, which is an important paleontol...
Ancient lake systems contain incredibly rich archives of past biological and environmental change. O...
We test several methods of ostracod-based palaeoenvironmental reconstruction using indicator species...
The University of Tübingen has a century old tradition of archaeological research on the Middle and ...
The sediments of the Slindon Formation at the junction of the Chalk South Downs and the West Sussex ...
The sediments of the Slindon Formation at the junction of the Chalk South Downs and the West Sussex ...
The sediments of the Slindon Formation at the junction of the Chalk South Downs and the West Sussex ...
2820 antler remains from the Lower Palaeolithic site of Bilzingsleben, Thuringia, Germany (excavatio...
The freshwater ostracods living exclusively in interstitial and/or interstitial and cavernous habita...
Ostracods as bioindicators are extremely useful for reconstructing palaeoenvironment and palaeoclima...
The Lower Palaeolithic, Middle Pleistocene locality Schöningen has been a focus of archaeological re...
Numerous fossil remains (vertebrates, molluscs and plants) were found in more than twenty sites of t...
Bilzingsleben is internationally known as a palaeontological, palaeoanthropological and archaeologic...
To trace environmental changes of the tectonically active Frasassi area in the northeastern Apennine...
none1noBenthic ostracod analyses performed on a 40 m long core (Core 1) enabled a detailed facies ch...
This thesis deals with the class Ostracoda from the Úpohlavy quarry, which is an important paleontol...
Ancient lake systems contain incredibly rich archives of past biological and environmental change. O...
We test several methods of ostracod-based palaeoenvironmental reconstruction using indicator species...
The University of Tübingen has a century old tradition of archaeological research on the Middle and ...
The sediments of the Slindon Formation at the junction of the Chalk South Downs and the West Sussex ...
The sediments of the Slindon Formation at the junction of the Chalk South Downs and the West Sussex ...
The sediments of the Slindon Formation at the junction of the Chalk South Downs and the West Sussex ...
2820 antler remains from the Lower Palaeolithic site of Bilzingsleben, Thuringia, Germany (excavatio...
The freshwater ostracods living exclusively in interstitial and/or interstitial and cavernous habita...
Ostracods as bioindicators are extremely useful for reconstructing palaeoenvironment and palaeoclima...
The Lower Palaeolithic, Middle Pleistocene locality Schöningen has been a focus of archaeological re...
Numerous fossil remains (vertebrates, molluscs and plants) were found in more than twenty sites of t...