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Paleoceanographic importance of tri- and di-unsaturated alkenones through the early phase of Cretaceous Oceanic Anoxic Event 2 from southern high latitudes of the proto-Indian Ocean
Organic Geochemistry ( IF 3 ) Pub Date : 2023-12-26 , DOI: 10.1016/j.orggeochem.2023.104722
Takashi Hasegawa , Akiko S. Goto

Alkenones are biomarkers derived exclusively from species of haptophyte algae. The relative abundance of di- to tri-unsaturated C37 alkenones expressed as UK'37 is widely applied as a sea surface paleotemperature proxy for Cenozoic marine sediments. However, the absence of alkatrienones prior to the Eocene has precluded application of the UK'37 proxy for assessment of Cretaceous paleoclimates. Herein, we report a C40 alkatrienone (tetraconta-9E, 16E, 23E-trien-3-one; C40:3 Et) in deep-sea sediments from southern high latitudes (International Ocean Discovery Program: IODP site U1516). This discovery extends the geologic record of alkatrienones to the late Cenomanian, ∼70 million years earlier than previous reports. The parallel occurrence of higher abundances of a C40 alkadienone (tetraconta-16E, 23E-dien-3-one; C40:2 Et) allowed calculation of the UK’40 unsaturation index, comparable to UK’37. Stratigraphic variations in the δ13C of C40:2 Et revealed an elevated (∼1.5 ‰) positive carbon isotope excursion (CIE) relative to those observed in carbonate from other OAE2 sequences likely reflecting a decrease in global pCO2. The UK’40 profile suggests a concurrent drop in sea surface temperature associated with the decline in pCO2 during the early phase of OAE2. The timing of these environmental perturbations in the southern high latitude of the proto-Indian Ocean suggests they were triggered by volcanism associated with large igneous province (LIP) formation.



中文翻译:

原印度洋南部高纬度白垩纪海洋缺氧事件 2 早期三不饱和烯酮和二不饱和烯酮的古海洋学重要性

烯酮是专门源自触生藻类物种的生物标志物。以 U K' 37表示的二至三不饱和 C 37烯酮的相对丰度被广泛用作新生代海洋沉积物的海面古温度代理。然而,始新世之前不存在链三烯酮,因此无法应用 UK ' 37代理来评估白垩纪古气候。在此,我们报告了南部高纬度地区深海沉积物中的 C 40链三烯酮(tetraconta-9 E、 16 E、 23 E -trien-3-one;C 40:3 Et)(国际海洋发现计划:IODP 站点 U1516) )。这一发现将链三烯酮的地质记录延伸至塞诺曼阶晚期,比之前的报道早约 7000 万年。较高丰度的 C 40链二烯酮(tetraconta-16 E、23 E -dien-3-one;C 40:2 Et)的并行出现允许计算 UK ' 40不饱和指数,与 UK ' 37相当。C 40:2 Et的 δ 13 C 的地层变化揭示了相对于其他 OAE2 序列碳酸盐中观察到的正碳同位素偏移 (CIE) 升高 (∼1.5 ‰),这可能反映了全球p CO 2的减少。U K' 40剖面表明,在 OAE2 早期阶段,海面温度同时下降,与p CO 2下降有关。原印度洋南部高纬度地区这些环境扰动的发生时间表明,这些环境扰动是由与大型火成岩省(LIP)形成相关的火山活动引发的。

更新日期:2023-12-26
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