Marine resource abundance drove pre-agricultural population increase in Stone Age Scandinavia.


Journal

Nature communications
ISSN: 2041-1723
Titre abrégé: Nat Commun
Pays: England
ID NLM: 101528555

Informations de publication

Date de publication:
24 04 2020
Historique:
received: 15 08 2019
accepted: 28 02 2020
entrez: 26 4 2020
pubmed: 26 4 2020
medline: 11 8 2020
Statut: epublish

Résumé

How climate and ecology affect key cultural transformations remains debated in the context of long-term socio-cultural development because of spatially and temporally disjunct climate and archaeological records. The introduction of agriculture triggered a major population increase across Europe. However, in Southern Scandinavia it was preceded by ~500 years of sustained population growth. Here we show that this growth was driven by long-term enhanced marine production conditioned by the Holocene Thermal Maximum, a time of elevated temperature, sea level and salinity across coastal waters. We identify two periods of increased marine production across trophic levels (P1 7600-7100 and P2 6400-5900 cal. yr BP) that coincide with markedly increased mollusc collection and accumulation of shell middens, indicating greater marine resource availability. Between ~7600-5900 BP, intense exploitation of a warmer, more productive marine environment by Mesolithic hunter-gatherers drove cultural development, including maritime technological innovation, and from ca. 6400-5900 BP, underpinned a ~four-fold human population growth.

Identifiants

pubmed: 32332739
doi: 10.1038/s41467-020-15621-1
pii: 10.1038/s41467-020-15621-1
pmc: PMC7181652
doi:

Types de publication

Historical Article Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

2006

Commentaires et corrections

Type : CommentIn
Type : CommentIn

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Auteurs

J P Lewis (JP)

Geography and Environment, Loughborough University, Loughborough, LE11 3TU, UK. J.P.Lewis@lboro.ac.uk.

D B Ryves (DB)

Geography and Environment, Loughborough University, Loughborough, LE11 3TU, UK.

P Rasmussen (P)

Environmental Archaeology and Materials Science, National Museum of Denmark, Brede Værk, I.C. Modewegsvej, DK-2800, Kgs. Lyngby, Denmark.

J Olsen (J)

Department of Physics and Astronomy, Aarhus University, Ny Munkegade 120, DK-8000, Aarhus C, Denmark.

L G van der Sluis (LG)

School of Natural and Built Environment, Queen's University Belfast, Belfast, BT7 1NN, UK.

P J Reimer (PJ)

School of Natural and Built Environment, Queen's University Belfast, Belfast, BT7 1NN, UK.

K-L Knudsen (KL)

Department of Earth Science, Aarhus University, Høegh-Guldbergs Gade 2, DK-8000, Aarhus C, Denmark.

S McGowan (S)

School of Geography, University of Nottingham, Nottingham, NG7 2RG, UK.

N J Anderson (NJ)

Geography and Environment, Loughborough University, Loughborough, LE11 3TU, UK.

S Juggins (S)

School of Geography, Politics and Sociology, Newcastle University, Newcastle upon Tyne, NE1 7RU, UK.

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