A 23.7-year long daily growth rate record of a modern giant clam shell from South China Sea and its potential in high-resolution paleoclimate reconstruction

2021 ◽  
Vol 583 ◽  
pp. 110682
Author(s):  
Nanyu Zhao ◽  
Hong Yan ◽  
Yuanjian Yang ◽  
Chengcheng Liu ◽  
Xiaolin Ma ◽  
...  
2021 ◽  
Vol 31 (11) ◽  
pp. 1655-1674
Author(s):  
Shengnan Zhou ◽  
Qi Shi ◽  
Hongqiang Yang ◽  
Xiyang Zhang ◽  
Xiaoju Liu ◽  
...  

2015 ◽  
Vol 83 (2) ◽  
pp. 298-306 ◽  
Author(s):  
Hong Yan ◽  
Liguang Sun ◽  
Da Shao ◽  
Yuhong Wang

Temperature seasonality, the difference between summer and winter temperature, has significant influences on global terrestrial and marine ecosystems. However, most of proxy-based climate records are of limited temporal resolution and thus insufficient to quantify the past temperature seasonality. In this study, high-resolution Sr/Ca ratios of modern (live-caught) and fossil (dead-collected) Tridacna gigas shells from the South China Sea (SCS) were used to reconstruct the seawater temperature seasonality during the late Holocene. The averaged seawater temperature seasonality around 2165 ± 75 BC (4.46 ± 1.41°C, derived from the data of 18 yr) were similar to the seasonality of recent decade (4.41 ± 0.82°C during AD 1994–2005), but the temperature seasonality around AD 50 ± 40 (3.69 ± 1.37°C, derived from the data of 48 yr) and AD 990 ± 40 (3.64 ± 0.87°C, derived from the data of 11 yr) was significantly lower than that during AD 1994–2005. The reduced seasonality around AD 990 ± 40 was attributable to the unusually warm winter during the medieval times, probably caused by the weakening of East Asian Winter Monsoon. Our study highlighted the potential of T. gigas shells in providing high-resolution seasonality climate information during the late Holocene.


2014 ◽  
Author(s):  
Donghong Luo ◽  
Ming Zhu ◽  
Wei Zhang ◽  
Ruiliang Wang ◽  
Xisheng Li ◽  
...  

2016 ◽  
Vol 176 ◽  
pp. 69-83 ◽  
Author(s):  
Yu-Shen Hsiao ◽  
Cheinway Hwang ◽  
Yung-Sheng Cheng ◽  
Liang-Chien Chen ◽  
Hung-Jui Hsu ◽  
...  

Author(s):  
Jaruwan Mayakun ◽  
Chen-Pan Liao ◽  
Shao-Lun Liu

Abstract Calcareous green alga in the genus Halimeda are important contributors to the marine carbonate budget. Dongsha Island is located in the northernmost South China Sea and is a seagrass-dominated ecosystem with intermixed Halimeda macroloba patches, making it an excellent system to better examine the extent of carbonate contribution by H. macroloba in such an ecosystem. To this end, we examined the standing stock and actual CaCO3 contribution of H. macroloba in the seagrass-dominated ecosystem (herein Dongsha Island) and compared them with those in Halimeda-dominated ecosystems. The density, growth rate, calcification rate and CaCO3 content of H. macroloba at four life stages were investigated. The mean density of H. macroloba was around 8.82 ± 1.57 thalli m−2 and the estimated standing stock was 61,740 to 72,730 thalli. Thalli produced 1 to 2 new segments day−1, giving a growth rate of 0.003 ± 0.001 g dry weight thallus−1 day−1. Calculated algal biomass and annual areal production were 0.03 g m−2 and 9.66 g m−2 year−1. In each square metre of this area, H. macroloba produced 8.82 to 17.64 new segments day−1, accumulating 0.002 ± 0.001 g CaCO3 thallus−1 day−1 or around 6.44 g CaCO3 m−2 year−1. Mean CaCO3 content was 0.32 ± 0.05 g thallus−1. As expected, the growth rate and CaCO3 production of H. macroloba in Dongsha Island were lower than in other studies from Halimeda tropical ecosystems. Overall, this work provides the baseline of carbonate production of H. macroloba in Dongsha Island and relevant systems where the ecosystem is dominated by seagrasses.


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