The influence and impact of tsunamis on the microorganism assembly of Nagatsura-Ura Lagoon, Miyagi, northeastern Japan

Two sediment cores were collected from two sites in Nagatsura-Ura Lagoon, the mouth of which was destroyed in the 2011 Tohoku-oki tsunami. Although sediment conditions differed widely between the central and inner parts of the lagoon, we could identify traces of the 2011 Tohoku-oki tsunami at both,...

Full description

Saved in:
Bibliographic Details
Published in:Fisheries science 2021-01, Vol.87 (1), p.121-130
Main Authors: Okumura, Yutaka, Matsuoka, Hiromi, Arakawa, Hisayuki, Tokanai, Fuyuki, Suzuki, Atsushi, Irizuki, Toshiaki, Kajita, Hiroto, Hara, Motoyuki
Format: Article
Language:English
Subjects:
Alliances
Biomedical and Life Sciences
Chlorophyll
Chlorophyll a
Composition
Cores
Diatoms
Dinoflagellates
Earthquakes
Fish & Wildlife Biology & Management
Food Science
Freshwater & Marine Ecology
Horizon
Lagoons
Life Sciences
Marine microorganisms
Microorganisms
Next-generation sequencing
Original Article
Phytoplankton
Plankton
Seawater
Sediment
Seismic activity
Tsunamis
Vertical profiles
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Two sediment cores were collected from two sites in Nagatsura-Ura Lagoon, the mouth of which was destroyed in the 2011 Tohoku-oki tsunami. Although sediment conditions differed widely between the central and inner parts of the lagoon, we could identify traces of the 2011 Tohoku-oki tsunami at both, and those of earlier tsunamis in the inner part of the lagoon. Chlorophyll  a maxima were observed at core depths between 62 and 72 cm in the central part of the lagoon. We inferred that this horizon correlated with the 2011 Tohoku-oki tsunami deposit. In the inner part of the lagoon, the horizon at core depths of 116—142 cm could be aged to the 1400s, and is thus thought to have been formed as a consequence of the Kyotoku earthquake of 1454. The dinoflagellate Alexandrium spp. accounted for ~ 22.6% of the total read numbers of phytoplankton from next generation sequencing. Diatoms made up the second largest group of phytoplankton, with Chaetoceros spp. representing ~ 10.5% of the total. The vertical profiles of dinoflagellate and diatom compositions showed little change. Although traces of tsunamis were observed in cores from the lagoon, and in nearby closed bays, we believe that the microbial composition has changed only slightly in the lagoon due to poor seawater exchange through the closed lagoon mouth.
ISSN:0919-9268
1444-2906
DOI:10.1007/s12562-020-01472-8