Images of salts of elements being ionized for isotopic measurements in a Thermal Ionization Mass Spectrometer hosted in Ramananda Chakrabarti’s lab at

Fish ear bones can reveal seawater temperature millions of years ago

INDIA
Friday, August 12, 2022, 07:00 (GMT + 9)

Researchers at the Indian Institute of Science (IISc) have now identified a way to estimate ancient seawater temperature by probing tiny bones in the ears of fish

Oceans cover three quarters of the earth's surface and host many remarkable life forms. Earth scientists have been attempting to reconstruct the seawater temperature over time, but it is not easy to do so.

Researchers at the Indian Institute of Science (IISc) have now identified a way to estimate ancient seawater temperature by probing tiny bones in the ears of fish. 

“When you go back in time, you don’t have any fossilised seawater,” explained Ramananda Chakrabarti, Associate Professor at the Centre for Earth Sciences (CEaS), IISc, and corresponding author of the study published in Chemical Geology. Therefore, he and his PhD student, Surajit Mondal, in collaboration with Prosenjit Ghosh, Professor at CEaS, turned to otoliths – tiny bones found in the inner ear of fish. 

An IISc release explained: "Like corals, otoliths are made of calcium carbonate and grow throughout a fish’s lifetime by accumulating minerals from seawater. Similar to tree rings, these otoliths also hold clues to the fish’s age, migration patterns, and the type of water that the fish lived in."

For several years, Prof. Chakrabarti and his team have been tracking calcium carbonate deposits found in tiny animals like corals or foraminifera. In the current study, they chose otoliths as scientists have discovered fossilised otolith samples dating as far back as the Jurassic period (172 million years ago).

Sampling locations of fish otoliths which were analysed for Sr/Ca, Mg/Ca, Ba/Ca, and δ 44/40 Ca in this study (modified from Ghosh et al., 2007).

The release said researchers used six present-day otolith samples collected from different geographical locations along the east coast of North America. They analysed the ratio of different calcium isotopes in these otoliths with a Thermal Ionisation Mass Spectrometer (TIMS). By measuring the ratios of calcium isotopes in the sample, they were able to correlate it with the seawater temperatures from which the fish were collected.

(a) The δ 44/40 Ca values in fish otolith samples show a positive correlation (r 2 = 0.86, p < 0.07) with water temperature and negative correlations with (b)

“We demonstrated that calcium isotopes are a powerful tracer of water temperature, and Surajit’s efforts make our lab the only lab in the country that can actually measure these isotopic variations,” Prof. Chakrabarti was quoted as saying. In addition to calcium isotopes, the team also analysed the concentration of other elements like strontium, magnesium, and barium, and their ratios in the same sample, and collated the data together to tease out a more accurate value for seawater temperature within a range of plus or minus one degree Celsius when compared to the actual value. 

(a) A strong negative correlation (r 2 = 0.8, p < 0.05) between δ 44/40 Ca and Sr/Ca suggests that simultaneous measurements of these two parameters in fish otoliths can be used for reliable paleotemperature reconstruction. In contrast, δ 44/40 Ca values show poor correlations with (b) Mg/Ca (r 2 = 0.56, p = 0.1) and (c) and Ba/Ca (r 2 = 0.58, p = 0.3) ratios, which suggests that factors other than temperature have a dominant control on the Mg and Ba incorporation in fish otoliths. The correlations were calculated excluding the Black drum sample BIO-6. 

Organisms that live in the ocean are extremely sensitive to temperatures. A two-degree temperature rise could lead to the extinction of several species. In addition, because the atmosphere and the ocean are “on talking terms”, a lot of the carbon dioxide in the atmosphere eventually dissolves into the ocean, and this ability is also linked to seawater temperature – the lower the temperature, the more carbon dioxide is trapped.

Because of the close correlation they found between calcium isotope ratios and temperatures, the authors are confident that their approach can now be used on fossilised samples. Mapping early seawater temperatures is important to better understand Earth’s history, they say. “What happened back in time is key to our understanding of what will happen in the future,”   Prof. Chakrabarti said.

Source: The Hindu

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