Oxygen isotopic variations in modern cetacean teeth and bones： implications for ecological, paleoecological, and paleoclimatic studies  

作　　者：Burcu Ciner Yang Wang William Parker 

机构地区：[1]Department of Earth,Ocean and Atmospheric Science,and National High Magnetic Field Laboratory,Florida State University,Tallahassee,FL,USA [2]Department of Geological Engineering,Balikesir University,Balikesir,Turkey [3]department of earth,ocean and atmospheric science,florida state university,Tallahassee,FL,USA

出　　处：《Science Bulletin》2016年第1期92-104,共13页科学通报（英文版）

基　　金：supported by US National Science Foundation Cooperative Agreement No.DMR-1157490 and the State of Florida;the State of Florida.The Stable Isotope Lab was established with grants from the US National Science Foundation(EAR-0824628;EAR-0517806 and EAR-0236357)

摘　　要：The oxygen isotope ratios （δ18O） preserved in marine sediments have been widely used to reconstruct past ocean temperatures. However, there remain significant uncertainties associated with this method, owing to assumptions about the δ18O of ancient seawater which affects the temperature inferred from sediment δ18O records. In this study, oxygen isotope compositions of phosphate in teeth and bones from five different modem cetacean species, including sperm whale, pygmy sperm whale, short-finned pilot whale, killer whale, and Cuvier＇s beaked whale, and three fossil whales were determined. The data were used to assess whether the oxygen isotope ratios of biogenic phosphate （δ18Op） from cetaceans are a reliable proxy for the oxygen isotopic composition of ocean water （δ18Ow）. The δ18Op values of modem cetaceans range from 15.5 ‰ to 21.3 ‰, averaging （19.6 ‰ ±0.8 ‰） （n = 136）.Using a greatly expanded global cetacean δ18Op dataset, the following regression equation is derived for cetaceans： δ18Ow = 0.95317 （4-0.03293） δ18Op- 17.971 （＋0.605）, r = 0.97253. The new equation, when applied to fossil teeth and bones, yielded reasonable estimates of ancient seawater δ18Ow values. Intra-tooth isotopic variations were observed within individual teeth. Among the selected species, the killer whale （O. orca） has largest intra-tooth δ18Op preference and migratory the lowest δ18Op values and the variation, reflecting its habitat behavior. The results show that oxygen isotope analysis of phosphate in cetacean teeth and dense ear bones provides a useful tool for reconstructing the oxygen isotopic composition of seawater and for examining environmental preferences （including migratory behavior） of both modem and ancient whales.The oxygen isotope ratios(d18O) preserved in marine sediments have been widely used to reconstruct past ocean temperatures. However, there remain significant uncertainties associated with this method, owing to assumptions about the d18 O of ancient seawater which affects the temperature inferred from sediment d18 O records. In this study, oxygen isotope compositions of phosphate in teeth and bones from five different modern cetacean species, including sperm whale, pygmy sperm whale, short-finned pilot whale, killer whale, and Cuvier's beaked whale, and three fossil whales were determined. The data were used to assess whether the oxygen isotope ratios of biogenic phosphate(d18Op) from cetaceans are a reliable proxy for the oxygen isotopic composition of ocean water(d18Ow). The d18 Opvalues of modern cetaceans range from15.5 % to 21.3 %, averaging(19.6 %± 0.8 %)(n = 136).Using a greatly expanded global cetacean d18 Opdataset, the following regression equation is derived for cetaceans:d18Ow= 0.95317(±0.03293) d18Op- 17.971(±0.605),r = 0.97253. The new equation, when applied to fossil teeth and bones, yielded reasonable estimates of ancient seawater d18 Owvalues. Intra-tooth isotopic variations were observed within individual teeth. Among the selected species, the killer whale(O. orca) has the lowest d18 Opvalues and the largest intra-tooth d18 Opvariation, reflecting its habitat preference and migratory behavior. The results show that oxygen isotope analysis of phosphate in cetacean teeth and dense ear bones provides a useful tool for reconstructing the oxygen isotopic composition of seawater and for examining environmental preferences(including migratory behavior)of both modern and ancient whales.

关 键 词：Oxygen isotopes PHOSPHATE CETACEAN WHALES Teeth Bones 

分 类 号：Q915[天文地球—古生物学与地层学] P736.22[生物学—古生物学]