Biology subjects

Kjaer, K. H.

Publications and source records attributed to Kjaer, K. H..

3 recordsLinked to original sources

bioRxiv2025

Environmental DNA Reveals Reykjavik's Human and Ecological History

Iceland was among the last large islands settled by humans, with colonization (Landnam) in the late 9th century CE (Common Era) and is often portrayed as an ecological disaster driven by the Norse settlers. Here, we revisit this narrative through environmental DNA (eDNA) and multiproxy analyses of sediment cores from Lake Tjornin in central Reykjavik, one of Icelands earliest and longest-occupied settlements. Originally a marine embayment, Tjornin became a freshwater lake around 660 CE. Our record reveals a human presence decades before the long-accepted arrival date of 877 CE, marked by the Landnam volcanic tephra. Early settlement brought livestock, barley cultivation, and other introduced taxa that enhanced nutrient cycling and unexpectedly increased local biodiversity. Contrary to the conventional view of rapid deforestation, eDNA shows that birch and willow expanded during the settlement period, likely supported by deliberate management. Pronounced ecological and land use shifts occurred after 1200 CE, but these were coeval with the Little Ice Age cooling, compounded by volcanic eruptions, storm surges, and plague, rather than anthropogenic degradation. Crop cultivation ceased, arboreal taxa retracted, and grazing pressure maintained open landscapes. Even more profound ecological changes came after c. 1750 CE with urbanization and industrialization, as wastewater discharge, heavy-metal pollution, and fossil fuel use reshaped Tjornins ecosystem. These findings challenge the prevailing model of Norse-induced environmental collapse, revealing instead a dynamic human-environment relationship shaped by both cultural practices and external stressors. By applying eDNA to a long-occupied urban catchment, we demonstrate the power of genomic methods to refine settlement chronologies, reassess ecological baselines and changes, and integrate natural and cultural histories. This approach offers a model for revisiting human-environment interactions in urban centers worldwide.

genomics↗

bioRxiv2023

A 2-million-year-old microbial and viral communities from the Kap Kobenhavn Formation in North Greenland

Environmental DNA (eDNA) from the 2-million-year-old Kap Kobenhavn Formation of northern Greenland has revealed an ecosystem of plants and animals with no contemporary analogue1. Here, we reconstruct the microbial (bacterial, archaeal, and viral) communities that thrived at the site during this time. By leveraging a novel analytical framework that integrates taxonomic profiling, DNA damage estimates, and functional reconstructions, we identify and distinguish pioneer microbial communities from later permafrost microbial assemblages. We show that at the time of sediment deposition, the terrestrial input at the Kap Kobenhavn site originated from a palustrine wetland, suggesting warmer, non-permafrost conditions. During this period, the detection of methanogenic archaea and signals of their carbon metabolism is consistent with Kap Kobenhavn and similar northern ecosystems contributing moderate methane emissions. Intriguingly, we discover a remarkable nucleotide sequence similarity--exceeding 98%--between pioneer methanogens and present-day analogues in thawing permafrost. This aligns with the concept of "time-traveling" microbes2 surviving across geological time and waiting for conditions to turn favourable rather than evolving to adapt to changing conditions. Importantly, in contrast to the plant and animal communities of the Kap Kobenhavn, a striking similarity in microbial composition to that of a contemporary thawing Arctic suggests that microbial communities may serve as the first indication of broader climate-driven ecosystem disruptions.

microbiology↗

bioRxiv2023

Importance of eDNA taphonomy and provenance for robust ecological inference: insights from interfacial geochemistry

Context for and purposeRetrieval of modern and ancient environmental DNA (eDNA) from sediments has revolutionized our ability to reconstruct present and past ecosystems. Little emphasis has been placed, however, on the fundamentals of the DNA-sediment associations and, consequently, our understanding of taphonomy and provenance of eDNA in sediments remains extremely limited. If we are to be able to accurately infer community dynamics across time and space from eDNA data, we need to understand how depositional processes and sedimentary associations of DNA molecules in different settings influence our interpretation. Approach and methodsHere, we introduce interfacial geochemical principles to the field of eDNA and discuss current interpretational biases. We outline a way to increase the scope and resolution of ecological interpretations from eDNA by combining mineralogic composition with experimental adsorption data. We apply distribution coefficients to assess the relationship between the DNA fraction in water columns and DNA fraction sequestered by suspended sediment particles. We further evaluate the challenges with drawing ecological inference using eDNA from sedimentary systems that receive input from different ecosystem types as a consequence of sedimentary processes. Main results: We show thatO_LIThe retention of DNA in aqueous environments depends on the mineralogy of sediment particles and on the number of particles loaded in the water column. C_LIO_LIDNA attached to sediment particles from distal systems can be deposited in proximal systems and skew the interpretation of the proximal sediment samples. C_LIO_LIHigh particle loading in the water column can deplete suspended DNA and cause inaccurate interpretation of aqueous DNA samples. C_LIO_LIHigh particle loading in surface sediment pore waters enhances sequestration of DNA from benthic communities relative to that of water column communities, resulting in skewed estimates of species richness and abundance from sedimentary DNA. C_LI We discuss how to integrate taphonomy and provenance knowledge into the reconstruction of modern and past ecosystems, and ecosystem monitoring from eDNA data. Conclusions and the wider implicationsOur findings demonstrate that integrating information about eDNA taphonomy and provenance into modern and past ecosystem reconstruction from eDNA data can enhance the scope, resolution and accuracy of our interpretations.

biochemistry↗