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Lars Stemmerik

Researcher at Geological Survey of Denmark and Greenland

Publications -  197
Citations -  3703

Lars Stemmerik is an academic researcher from Geological Survey of Denmark and Greenland. The author has contributed to research in topics: Permian & Cretaceous. The author has an hindex of 30, co-authored 193 publications receiving 3309 citations. Previous affiliations of Lars Stemmerik include Natural History Museum & University of Copenhagen.

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Book ChapterDOI

The Permian of the Western Margin of the Greenland Sea—A Future Exploration Target

TL;DR: The Upper Permian of central East Greenland contains a relatively thick, widely distributed, oil-prone source rock It occurs directly adjacent to large, carbonate buildups that constitute the main potential reservoirs It is immediately overlain by thick, coarse-grained sandstones that are also a potential reservoir.
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Late Palaeozoic evolution of the North Atlantic margin of Pangea

TL;DR: In this article, 11 palaeogeographic maps spanning the earliest Carboniferous (Tournaisian) to Late Permian (Kazanian) have been constructed for the northern North Atlantic, based on available onshore and offshore data.
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Upper Campanian–Maastrichtian nannofossil biostratigraphy and high-resolution carbon-isotope stratigraphy of the Danish Basin: Towards a standard δ13C curve for the Boreal Realm

TL;DR: In this paper, the Campanian-Maastrichtian boundary (CMB) is identified through the correlation of dinoflagellate biostratigraphy and δ13C stratigraphy between Stevns-1 and the Global boundary Standard Stratotype-section and Point at Tercis les Bains (SW France).
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Upper Campanian–Maastrichtian holostratigraphy of the eastern Danish Basin

TL;DR: In this article, a high-resolution holostratigraphic analysis of this part of the Chalk Group has been undertaken on these cores, notably Stevns-1, in order to provide a record of changes in chalk facies, water depths and sea-water temperatures.
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Late Cretaceous (late Campanian–Maastrichtian) sea-surface temperature record of the Boreal Chalk Sea

TL;DR: In this paper, the authors presented a record of very high-resolution (ca. 4.5 kyr) sea-surface temperature (SST) changes from the Boreal epicontinental Chalk Sea (Stevns-1 core, Denmark), tied to an astronomical timescale of the late Campanian-Maastrichtian (74 to 66 Ma).