Dataset

   File(s) held in another repository
Title of Dataset
Data from: Response of deep-sea biodiversity to abrupt deglacial and Holocene climate changes in the North Atlantic Ocean
Author of Dataset
Okahashi, Hisayo1
Cronin, Thomas M.2
Rasmussen, Tine L.3
Hunt, Gene4
Contact
Yasuhara, Moriaki1
Date of Dataset Creation
2014-04-25
Description
Aim: Little is known about how marine biodiversity responds to oceanographic and climatic changes over the decadal to centennial time-scales which are most relevant for predicted climate changes due to greenhouse gas forcing. This paper aims to reveal decadal–centennial scale deep-sea biodiversity dynamics for the last 20,000 years and then explore potential environmental drivers. Location: The North Atlantic Ocean. Methods: We investigated deep-sea benthic microfossil records to reveal biodiversity dynamics and subsequently applied comprehensive ecological modelling to test possible environmental factors (i.e. surface productivity, seasonality of productivity or deepwater circulation related to bottom-water temperature) that may have influenced deep-sea biodiversity over these time-scales. Results: Deep-sea biodiversity changed synchronously with stadial–interstadial climate changes over the last 20,000 years across a large area of the North Atlantic in both ostracod crustaceans and foraminiferan protozoa (in spite of their different dispersal abilities). Species diversity rapidly increased during abrupt stadial events during the last deglacial and the Holocene interglacial periods. These include the well-known Heinrich 1, the Younger Dryas and the 8.2 ka events when the strength of Atlantic Meridional Overturning Circulation (AMOC) decreased. There is also evidence for quasi-cyclic changes in biodiversity at a c. 1500-year periodicity, consistent with the well-known ‘1500-year climatic cycle’. Statistical analyses revealed that AMOC variability (probably specifically the variability in AMOC-driven bottom-water temperature) is correlated with deep-sea biodiversity. Main conclusions: Our finding of a significant AMOC–diversity relationship may indicate pervasive control of the diversity of deep-sea benthic species by rapidly changing climate, specifically bottom-water temperature, over decadal to centennial time-scales. Our results, based on highly resolved fossil records, may portend pervasive, synchronous and sudden ecosystem responses to human-induced changes to climate and ocean circulation in this century.
Citation
Yasuhara, M, Okahashi, H, Cronin, TM, Rasmussen, TL, Hunt, G. (2014). Data from: Response of deep-sea biodiversity to abrupt deglacial and Holocene climate changes in the North Atlantic Ocean. [Data File]. Access to Files at http://dx.doi.org/10.5061/dryad.53vs3
Subject (RGC Codes)
M1 — Biological Sciences — 生物科學
  • 1105 — Ecology — 生態學
Subject (ANZSRC)
06 — BIOLOGICAL SCIENCES — 生物科學
  • 0602 — ECOLOGY — 生態學
    • 060205 — Marine and Estuarine Ecology (incl. Marine Ichthyology) — 海洋與河口生態
Keyword
Abrupt climate change
decadal–centennial time-scales
deep sea
deepwater circulation
macroecology
paleoecology
species diversity
temperature
Affiliations
  1. Univ Hong Kong, Sch Biol Sci, Swire Inst Marine Sci, Hong Kong, Hong Kong, Peoples R China ; Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China
  2. US Geol Survey, Reston, VA 20192 USA
  3. Univ Tromso, Dept Geol, N-9037 Tromso, Norway
  4. Smithsonian Inst, Natl Museum Nat Hist, Dept Paleobiol, Washington, DC 20013 USA