Evidence map›Paper›PMID 37068242›Full record

ArticleProceedings of the National Academy of Sciences of the United States of America2023

Sea-level rise in Southwest Greenland as a contributor to Viking abandonment.

Marisa Borreggine, Konstantin Latychev, Sophie Coulson, Evelyn M Powell, Jerry X Mitrovica, Glenn A Milne, Richard B Alley

Abstract read
In one paragraph

Article in Proceedings of the National Academy of Sciences of the United States of America, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.

0numbers the graph read from it
0cells of the map it votes in
3citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

3 citing papers in PubMed.

  1. Article
  2. Article
  3. Sea-level rise in Southwest Greenland as a contributor to Viking abandonment.Proceedings of the National Academy of Sciences of the United States of America · 2023
    Article
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

7 authors.

Marisa BorreggineDepartment of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138.ORCID 0000-0001-6015-8721
Konstantin LatychevDepartment of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138.ORCID 0000-0002-9970-9129
Sophie CoulsonDepartment of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138.ORCID 0000-0001-9353-2054
Evelyn M PowellDepartment of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138.ORCID 0000-0001-7661-5878
Jerry X MitrovicaDepartment of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138.
Glenn A MilneDepartment of Earth and Environmental Sciences, University of Ottawa, Ottawa, ON K1N 6N5, Canada.ORCID 0000-0002-5498-9403
Richard B AlleyDepartment of Geosciences, and Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA 16802.ORCID 0000-0003-1833-0115

Funding

Heising-Simons Foundation (HSF) 2018-0769NASA | Earth Sciences Division (NASA Earth Science Division) 80NSSC21K1790
6 · The paper itself

Abstract

The first records of Greenland Vikings date to 985 CE. Archaeological evidence yields insight into how Vikings lived, yet drivers of their disappearance in the 15th century remain enigmatic. Research suggests a combination of environmental and socioeconomic factors, and the climatic shift from the Medieval Warm Period (~900 to 1250 CE) to the Little Ice Age (~1250 to 1900 CE) may have forced them to abandon Greenland. Glacial geomorphology and paleoclimate research suggest that the Southern Greenland Ice Sheet readvanced during Viking occupation, peaking in the Little Ice Age. Counterintuitively, the readvance caused sea-level rise near the ice margin due to increased gravitational attraction toward the ice sheet and crustal subsidence. We estimate ice growth in Southwestern Greenland using geomorphological indicators and lake core data from previous literature. We calculate the effect of ice growth on regional sea level by applying our ice history to a geophysical model of sea level with a resolution of ~1 km across Southwestern Greenland and compare the results to archaeological evidence. The results indicate that sea level rose up to ~3.3 m outside the glaciation zone during Viking settlement, producing shoreline retreat of hundreds of meters. Sea-level rise was progressive and encompassed the entire Eastern Settlement. Moreover, pervasive flooding would have forced abandonment of many coastal sites. These processes likely contributed to the suite of vulnerabilities that led to Viking abandonment of Greenland. Sea-level change thus represents an integral, missing element of the Viking story.

Indexed as

archaeologyglacial isostatic adjustmentNorsesea-level change

Identifiers

PMID37068242
PMCPMC10151458

What OpenQuestion holds

Textmetadata
LicenceCC BY-NC-ND
Read underepoch 390

Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.