• 検索結果がありません。

南極海生態系の応答を通して探る地球環境変動-

N/A
N/A
Protected

Academic year: 2021

シェア "南極海生態系の応答を通して探る地球環境変動-"

Copied!
1
0
0

読み込み中.... (全文を見る)

全文

(1)

南極海生態系の応答を通して探る地球環境変動-JARE53報告-

佐々木洋1、秋葉文弘1、本川正三2、栗原晴子3、遠藤 寿5、吉川久幸5、飯田高弘6 橋田 元6、小達恒夫6、服部寛7

1:石巻専修大学、2:創価大学、3:琉球大学、5:北海道大学、6:極地研究所、7:東海大学

Responses of Antarctic marine ecosystems to global environmental changes with carbonate systems (RAMEEC) – Preliminary report of JARE53 -

Hiroshi Sasaki

1

, Fumihiro Akiha

1

, Shozo Motokawa

2

, Haruko Kurihara

3

, Hisashi Endo

5

, Hisayuki Yoshikawa

5

, Takahiro Iida

6

, Gen Hashida

6

, Tsuneo Odate

6

, Hiroshi Hattori

7

1: Senshu U. Ishinomaki, 2: Soka U., 3: Ryukyu U., 4: Tohoku U., 5: Hokkaido U., 6: NIPR, 7: Tokai U.

The present study focuses on responses of Antarctic marine ecosystems to global environmental changes with special reference to ocean acidification. The target sea area was primarily 40-65

o

S along 110

o

E in the Indian Sector of the Southern Ocean (Fig 1). Successive oceanographic observations were made in early December with the icebreaker “Shirase”, from late December to late-January with “Umitaka-maru”, and in early March again with “Shirase”. Intensive studies on spatio-temporal distributions of carbonates, distributions and abundances of phytoplankton and shelled pteropods, influences of acidified seawater to phytoplankton and shelled pteropods were carried out on board the “Umitaka-maru”. Surface drifters with multiple sensors and GPS was deployed at 60

o

S, 110

o

E and 62

o

S, 110

o

E for about 3 weeks, and a bottom-tethered sediment trap array was recovered at the same site (4100m depth). I will show the outline of above mentioned studies.

Fig. 1. Cruise track of JARE53 in the study sea area of the Southern Ocean.

本研究の目的は、大気中二酸化炭素濃度増加に伴う海洋酸性化などの変化が南極海の生態系に与える影響を解 明することである。主な観測海域は夏季の南大洋インド洋区の

110

o

E

線に沿って

40-65

o

S

付近である。JARE53 おける観測は昨年度

JARE52

においてとほぼ同様に実施された。

12

月初旬に「しらせ」が

110

o

E

線を南下通過時 に数点の定点観測と表層係留系の投入(60o

S, 110

o

E

および

62

o

S, 110

o

E)が行われ、12

月下旬から

1

月初旬にかけ て「海鷹丸」航海中に集中的な定点観測、および表層係留系の回収が行われた。昨年度設置された海底設置型の 深層係留系(60o

S, 110

o

E)は回収された。3

月初旬に再び「しらせ」が

60

o

S, 110

o

E

付近を西進通過時においても観 測が実施された。主な観測項目は、海水中の溶存炭酸の時空間分布、植物プランクトン群の分布、植物プランク トンに対する酸性化海水の影響、また有殻翼足類の分布生態、翼足類に対する酸性化海水の影響などである。こ れらの結果の概要について紹介する。

Fig. 1. Cruise track of JARE53 in the study sea area of the Southern Ocean.

参照

関連したドキュメント

We argue inductively for a tree node that the graph constructed by processing each of the child nodes of that node contains two root vertices and that these roots are available for

Polynomials (2.1) satisfy the following very useful identity originally formulated for so called contin- uous q − Hermite polynomials h n (can be found in e.g.. First assertions

In [9], it was shown that under diffusive scaling, the random set of coalescing random walk paths with one walker starting from every point on the space-time lattice Z × Z converges

Shen, “A note on the existence and uniqueness of mild solutions to neutral stochastic partial functional differential equations with non-Lipschitz coefficients,” Computers

Here we shall supply proofs for the estimates of some relevant arithmetic functions that are well-known in the number field case but not necessarily so in our function field case..

The unpublished data used in the economical evaluation corresponded to the diameter at breast height of 10 m height mature gray birch trees collected in 2004, which are part of

A connection with partially asymmetric exclusion process (PASEP) Type B Permutation tableaux defined by Lam and Williams.. 4

【おかやまビーチスポーツフェスティバルの目的】