冲绳海槽中部8.2ka以来GDGTs组成及温度重建*

doi:10.11978/2019090

Abstract

Abstract:

The wide occurrence of isoprenoid glycerol dibiphytanyl glycerol tetraethers (isoGDGTs) and its sensitivity to temperature in marine environments proved to be suitable for paleo-climate studies. The Okinawa Trough (OT), under the control of multiple climate patterns and various sediment origins, is a natural laboratory for paleo-climate study since the Holocene. Here, we studied isoGDGTs composition and characteristics, applied outspread tetraether index of tetraethers consisting of 86 carbons (TEX^H₈₆ index), tried to identify the source of isoGDGTs, and quantificationally discussed sea surface temperature (SST) of the central OT for the past 8.2 ka BP. By calculating the Methane Index and the branched isoprenoid tetraether (BIT) indexes, we found isoGDGTs mainly came from Thaumarchaeota, and are suitable for TEX^H₈₆ appliance. TEX^H₈₆ SST of column C14 revealed a range of 21.6-27.2 °C during 8.2 ka BP. Changes in SSTs of the central OT were primarily controlled by the western tropical Pacific Ocean and low-latitude winter insolation. The warming TEX^H₈₆ SSTs in the central OT were decoupled from the descending East Asian summer monsoon intensity in the last 8.2 ka BP. The widely recorded cold event at 7.4-6.6 ka BP was magnified in GDGTs related SST. We attributed it to the well-known Kikai-Akahoya tephra (~7.3 ka BP).

Key words: Isoprenoid glycerol dibiphytanyl glycerol tetraethers (isoGDGTs), TEX^H₈₆ proxy, sea surface temperature, the central Okinawa Trough

CLC Number:

P532

LIU Lei, XU Lanfang, GUAN Hongxiang, SUN Zhilei, WANG Libo, MAO Shengyi, LIU Lihua, WU Nengyou. The source of glycerol dibiphytanyl glycerol tetraethers and temperature reconstruction since 8.2 ka in the central Okinawa Trough[J].Journal of Tropical Oceanography, 2020, 39(6): 77-92.

Figures/Tables 9

Fig. 1

Tab. 1

Definitions of various proxies used in this article"

指标定义*	合理范围	来源
$\text{TE}{{\text{X}}_{86}}=\frac{\text{( }\!\![\!\!\text{ GDGT-2 }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-3 }\!\!]\!\!\text{ + }\!\![\!\!\text{ Crenarchaeol regio isomer }\!\!]\!\!\text{ )}}{\text{( }\!\![\!\!\text{ GDGT-1 }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-2 }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-3 }\!\!]\!\!\text{ + }\!\![\!\!\text{ Crenarchaeol regio isomer }\!\!]\!\!\text{ )}}$		Schouten et al, 2002
$\text{TEX}_{\text{86}}^{\text{H}}=\log (\text{TE}{{\text{X}}_{86}})$	>15℃	Kim et al, 2010
$\text{TEX}_{\text{86}}^{\text{L}}=\log \left( \frac{\text{ }\!\![\!\!\text{ GDGT-2 }\!\!]\!\!\text{ }}{\text{ }\!\![\!\!\text{ GDGT-1 }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-2 }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-3 }\!\!]\!\!\text{ }} \right)$	<15℃	Kim et al, 2010
$\text{BIT}=\frac{\text{ }\!\![\!\!\text{ GDGT-Ia }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-IIa }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-IIIa }\!\!]\!\!\text{ }}{\text{ }\!\![\!\!\text{ GDGT-Ia }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-IIa }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-IIIa }\!\!]\!\!\text{ + }\!\![\!\!\text{ Crenarchaeol }\!\!]\!\!\text{ }}$	<0.4	Hopmans et al, 2004
$\text{MI}=\frac{\text{ }\!\![\!\!\text{ GDGT-1 }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-2 }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-3 }\!\!]\!\!\text{ }}{\text{ }\!\![\!\!\text{ GDGT-1 }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-2 }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-3 }\!\!]\!\!\text{ + }\!\![\!\!\text{ Crenarchaeol }\!\!]\!\!\text{ + }\!\![\!\!\text{ Crenarchaeol regio isomer }\!\!]\!\!\text{ }}$	<0.3	Zhang et al, 2011
$\text{ }\!\!%\!\!\text{ GDGT-2}=\frac{\text{GDGT-2}}{\text{ }\!\![\!\!\text{ GDGT-1 }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-2 }\!\!]\!\!\text{ + }\!\![\!\!\text{ GDGT-3 }\!\!]\!\!\text{ + }\!\![\!\!\text{ Crenarchaeol regio isomer }\!\!]\!\!\text{ }}$	<45	Sinninghe Damsté et al, 2012
[GDGT-0] / [Crenarchaeol]	<2	Blaga et al, 2009
[GDGT-2] / [Crenarchaeol]	<0.4	Weijers et al, 2011

Tab. 1

Fig. 2

Tab. 2

Fig. 3

Tab. 3

Fig. 4

Fig. 5

Fig. 6

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Beta实验室编号	深度/(cm bsf)	平均深度/(cm bsf )	有孔虫种类	传统¹⁴C年龄/(a BP)	2σ校正年龄/(a BP)	平均校正年龄/(a BP)
498910	35~37.5^b	36.25	G.ruber, G.sacculifer	1100±30 ^a	616—730	673
498912	155~157.5^b	156.25	G.ruber, G.sacculifer	2330±30	1858—2045	1951.5
498914	365~367.5^b	366.25	G.ruber,,G.sacculifer	4790±30	4943—5227	5085
498915	455~457.5^c	456.25	G.ruber, G.sacculifer	6280±30	6831—6646	6738.5
498916	545~547.5^c	546.25	G.ruber, G.sacculifer	6940±30	7520—7385	7452.5
498917	575~577.5^c	576.25	G.ruber, G.sacculifer	7780±30	8170—8327	8248.5

The source of glycerol dibiphytanyl glycerol tetraethers and temperature reconstruction since 8.2 ka in the central Okinawa Trough

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