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Reconstructing extreme climatic and geochemical conditions during the largest natural mangrove dieback on record

Sippo, J. Z. (author)
Santos, Isaac R. (author)
Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences
Sanders, C. J. (author)
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Gadd, P. (author)
Hua, Q. (author)
Lovelock, C. E. (author)
Santini, N. S. (author)
Johnston, S. G. (author)
Harada, Y. (author)
Reithmeir, G. (author)
Maher, D. T. (author)
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 (creator_code:org_t)
2020-09-28
2020
English.
In: Biogeosciences. - : Copernicus GmbH. - 1726-4170 .- 1726-4189. ; 17:18, s. 4707-4726
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • A massive mangrove dieback event occurred in 2015-2016 along similar to 1000km of pristine coastline in the Gulf of Carpentaria, Australia. Here, we use sediment and wood chronologies to gain insights into geochemical and climatic changes related to this dieback. The unique combination of low rainfall and low sea level observed during the dieback event had been unprecedented in the preceding 3 decades. A combination of iron (Fe) chronologies in wood and sediment, wood density and estimates of mangrove water use efficiency all imply lower water availability within the dead mangrove forest. Wood and sediment chronologies suggest a rapid, large mobilization of sedimentary Fe, which is consistent with redox transitions promoted by changes in soil moisture content. Elemental analysis of wood cross sections revealed a 30- to 90-fold increase in Fe concentrations in dead mangroves just prior to their mortality. Mangrove wood uptake of Fe during the dieback is consistent with large apparent losses of Fe from sediments, which potentially caused an outwelling of Fe to the ocean. Although Fe toxicity may also have played a role in the dieback, this possibility requires further study. We suggest that differences in wood and sedimentary Fe between living and dead forest areas reflect sediment redox transitions that are, in turn, associated with regional variability in groundwater flows. Overall, our observations provide multiple lines of evidence that the forest dieback was driven by low water availability coinciding with a strong El Nino-Southern Oscillation (ENSO) event and was associated with climate change.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)

Keyword

salt-marsh dieback
el-nino events
growth rings
drought
radiocarbon
sediments
forests
distributions
frequency
dynamics
Environmental Sciences & Ecology
Geology

Publication and Content Type

ref (subject category)
art (subject category)

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