Terrigenous dissolved organic matter persists in the energy-limited deep groundwaters of the Fennoscandian Shield. [PDF]
Nat Commun, 2022 Dissolved organic matter in the Fennoscandian Shield deep continental bedrock fracture waters of varying characteristics and ages carries a strong terrigenous signature, and only a small proportion of this potential energy source links to the deep ...
Osterholz H +6 more
europepmc +2 more sources
Connectivity of Fennoscandian Shield terrestrial deep biosphere microbiomes with surface communities. [PDF]
Commun Biol, 2022 Westmeijer et al. employ high-throughput sequencing to investigate the connection between deep biosphere groundwaters and surface microbial communities.
Westmeijer G +10 more
europepmc +2 more sources
Deep seismic studies in the southeastern Fennoscandian Shield
Geofizicheskiy Zhurnal, 2017 The modern concept of the deep structure of the earth crust of the Ladoga-Bothnian zone, based on analysis and summing-up of all available information obtained in the last 35 years, is presented. Tomographic models were constructed, our concepts of the stratification of the earth crust and the geometry of seismic boundaries were revised and the ...
N. Sharov
openaire +4 more sources
, 2018 The presence of high mountains along passive margins is not unusual, as shown by their presence in several regions (Scandinavia, Greenland, East US, SW Africa, Brazil, West India and SE Australia).
Richard W. England (5149115) +3 more
core +15 more sources
Energy efficiency and biological interactions define the core microbiome of deep oligotrophic groundwater. [PDF]
Nat Commun, 2021 Ecological constraints on microbial niches in oligotrophic deep groundwaters remain elusive. This study provides support for the existence of a common core microbiome in two deep groundwater biomes of the Fennoscandian Shield using a genome-resolved ...
Mehrshad M +8 more
europepmc +2 more sources
Precambrian geodynamics and ore formation : the Fennoscandian Shield
, 2006 The complex geodynamic evolution of the Fennoscandian Shield from 2.06 to 1.78 Ga involved rapid accretion of island arcs and several microcontinent-continent collisions in a complex array of orogens. With a few exceptions, all major ore deposits formed in specific tectonic settings between 2.06 and 1.78 Ga and thus a strong geodynamic control on ore ...
Weihed, Pär +7 more
core +4 more sources
Archean and proterozoic gold deposits of the Fennoscandian shield
, 2008 Validerat; 20101217 (root)
Lukonin, Dmitry
core +4 more sources
The Fennoscandian Shield within Fennoscandia [PDF]
Bulletin of the Geological Society of Finland, 1996 J. Donner
openaire +2 more sources
The Fennoscandian Shield deep terrestrial virosphere suggests slow motion 'boom and burst' cycles. [PDF]
Commun Biol, 2021 Karin Holmfeldt et al. sequence metagenomes and metatranscriptomes of viruses in deep groundwaters down to 448 m below the surface. The results reveal ecological dynamics of viruses including slow motion ‘boom and burst’ cycles and a ‘kill the winner ...
Holmfeldt K +9 more
europepmc +2 more sources
Seismic model of the Earth's crust and upper mantle beneath the Fennoscandian Shield [PDF]
E3S Web of Conferences, 2023 Well-founded concepts of the crust and upper mantle structure of the Fennoscandian Shield were developed. Quantitative evidence for horizontal and vertical lithospheric heterogeneities was obtained.
Lebedev Artem, Sharov Nikolay
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