Cohen Anne L, Owens Kathryn E, Layne Graham D, Shimizu Nobumichi
Department of Geology and Geophysics, Woods Hole Oceanographic Institution (WHOI), Woods Hole, MA 02543, USA.
Science. 2002 Apr 12;296(5566):331-3. doi: 10.1126/science.1069330. Epub 2002 Mar 7.
The strontium-to-calcium ratio (Sr/Ca) of reef coral skeleton is commonly used as a paleothermometer to estimate sea surface temperatures (SSTs) at crucial times in Earth's climate history. However, these estimates are disputed, because uptake of Sr into coral skeleton is thought to be affected by algal symbionts (zooxanthellae) living in the host tissue. Here, we show that significant distortion of the Sr/Ca temperature record in coral skeleton occurs in the presence of algal symbionts. Seasonally resolved Sr/Ca in coral without symbionts reflects local SSTs with a temperature sensitivity equivalent to that of laboratory aragonite precipitated at equilibrium and the nighttime skeletal deposits of symbiotic reef corals. However, up to 65% of the Sr/Ca variability in symbiotic skeleton is related to symbiont activity and does not reflect water temperature.
珊瑚礁骨骼的锶钙比(Sr/Ca)通常被用作古温度计,以估算地球气候历史关键时期的海面温度(SST)。然而,这些估算存在争议,因为人们认为锶被吸收到珊瑚骨骼中会受到生活在宿主组织中的藻类共生体(虫黄藻)的影响。在这里,我们表明,在存在藻类共生体的情况下,珊瑚骨骼中Sr/Ca温度记录会出现显著扭曲。没有共生体的珊瑚中按季节解析的Sr/Ca反映了当地的SST,其温度敏感性与在平衡状态下沉淀的实验室文石以及共生珊瑚礁珊瑚的夜间骨骼沉积物相当。然而,共生骨骼中高达65%的Sr/Ca变异性与共生体活动有关,并不反映水温。