The Paleocene bird Scaniornis was described from fossil bones aged some 60 million years or more, which were found in the Limnhamn limestone; it was apparently a waterbird and might have been an early flamingo relative.
Situated a bit southwestwards — between 44° and 54° North — of its present location due to plate tectonics, in a fairly wet and warm epoch, the region had probably a warm-temperate to subtropical and fairly humid climate, altogether not too dissimilar from today's Black Sea region or French Mediterranean.
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Thus, it would seem to have been a native of the prehistoric North Sea, which at that time covered part of today's Germany and France, and sometimes was cut off from the Tethys and Atlantic Oceans, sometimes connected to them, and sometimes even to the Turgai Sea.