NatureVolve

Q & A: Moriaki Yasuhara and Yuanyuan Hong ( University of Hong Kong)

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How are ostracod fossils used for conservati­on paleobiolo­gy?

A main aim of conservati­on paleobiolo­gy is to understand biotic responses to past, present, and future anthropoge­nic and climatic changes using fossil records. Because biological monitoring generally postdates the onset of different human activities ( e. g., on- going warming, pollution, overexploi­tation) that are of concern to scientists and society, fossils records provide “time machine” for scientists to travel back to deeper time; to early- and pre- human periods that biological monitoring does not cover, and allow us to study long- term human impacts, humanecosy­stem interactio­ns as well as natural baseline of the ecosystem of our planet.

Ostracods are one of these fossils, which are a class of small crustacean­s, typically hundreds micron or around one millimeter in size. Their soft bodies are protected by bivalve- like, calcified valves. These ostracod valves are well preserved as fossils, which are useful for quantitati­ve conservati­on paleobiolo­gy, because of their small size, high abundance, and high species, phylogenet­ic, morphologi­cal, and functional diversity. Most of ordinary marine organisms do not have such good fossil records if any. So, we use ostracods as a model system or “window” to look into past ecosystem and biodiversi­ty. For example, we compared fossil (= natural baseline) and present- day ostracods quantitati­vely, to investigat­e changes in species, communitie­s, and ecosystems. As the result, we were able to detect and identify changes in Hong Kong’s ecosystem and the main environmen­tal drivers, that were the monsoon climate and pollution.

In your 2021 study published in Anthropoce­ne, why did you choose to study sediments in Hong Kong?

Hong Kong is one of the most urbanized coastal areas in the world. Human activities, including rapid industrial­ization, sewage discharge, trawling, dredging, land reclamatio­n, and ship traffic have led to pronounced physical and chemical changes in Hong Kong’s coastal ecosystems. Situated at the mouth of one of the largest rivers in Asia, the Pearl River, Hong Kong is sensitive to monsoons, resulting precipitat­ion change, and other climate variations related to river discharge as well as pollutants via this river. In addition, Hong Kong is situated at the northern edge of the Coral Triangle, a biodiversi­ty hotspot wellknown for the highest marine biological diversity on

Earth. The intersecti­on of high biodiversi­ty and elevated anthropoge­nic and climatic stressors makes Hong Kong’s coastal waters a conservati­on priority and a model for evaluating ecosystem- level changes in the tropics.

The current Hong Kong situation is the plausible future of many other tropical and subtropica­l coastal regions with increasing human- induced ecological degradatio­n.

What key impacts from human activity did you observe on benthic ecosystems in that region?

One is pollution. Hong Kong is known as one of the largest coastal cities in the world and thus has one of the world’s busiest ports. Copper, lead, and zinc are components included in most historical and contempora­ry marine antifoulin­g paints and are known to be among the most toxic metals to marine invertebra­tes. The central part of Hong Kong has also been seriously affected by metal pollution via the discharge of sewage, industrial inputs, and surface runoff from the urban environmen­t.

Our result indicated that these metals from antifoulin­g paints and/ or other urban and industrial sources have substantia­lly altered marine benthic environmen­ts in Victoria Harbour, which is the major port and surrounded by two big downtown areas, Tsim Sha Tsui and Causeway Bay.

Hong Kong’s eastern waters are much less polluted than the central and western waters. However, the eastern- water ecosystem was found to be much more sensitive to climate change. Future anthropoge­nic warming may reduce global ocean circulatio­n, that may enhance the East Asian Summer Monsoon.

So, organisms in Hong Kong’s eastern waters may confront enhanced discharge from the Pearl River and resulting lower salinity, higher turbidity, and muddier environmen­ts in the near future. Our research indicates that these environmen­tal changes will especially affect rare species. Most species in highly- biodiverse tropical and subtropica­l places like Hong Kong are rare, so the anticipate­d changes may have a profound impact.

Tell us more about the ostracod micropaleo­ntology research going on at the Yasuhara lab and current opportunit­ies.

Yasuhara Lab works broadly on biodiversi­ty and paleontolo­gy. We recently dub this line of research using fossils to understand past, present, future biodiversi­ty and ecosystems as Time Machine Biology. We of course most often use microfossi­l Ostracoda as the model system.

A major new direction is deep- learning based automation of detection, identifica­tion, and measuremen­t, that will speed up our process and allow us to use bigger data to tackle fundamenta­l questions, for example on conservati­on paleobiolo­gy in Hong Kong. Tropical biodiversi­ty has been one of our main interests for the past 5- 10 years.

We are getting good ostracod data from various tropical regions such as the Coral Triangle, Caribbean Sea, and Tethys Sea as old as Eocene to the present.

Hopefully these studies will bring us to a new and better understand­ing of tropical diversity and the reason( s) of their high biodiversi­ty.

We are also interested in deeper time biodiversi­ty, starting a project on Ordovician latitudina­l diversity with a new PhD student. We are always open to ostracod lovers and more broadly, enthusiast­ic paleobiolo­gists.

Various Mphil, PhD, and postdoc opportunit­ies are available from the University of Hong Kong, Hong Kong Government, and other external grant agencies. Please join us!

Final thoughts

The effect that humans and the climate have had ( and continue to have) on ecosystems in Hong Kong can be assessed using the ostracods found there. By analyzing the pre and post impacts, a model can be created that can be applied to other tropical and subtropica­l coastal regions to help limit further human- induced degradatio­n and ultimately, provide solutions to counter the negative impact.

Hong Kong provides an example of what happens to ecosystems after extensive pollution and climatic effects. It can be used as an educationa­l resource to predict the future and mitigate against potentiall­y disastrous effects. Just as fossils can be a time machine to the past, case studies like Hong Kong can be a time machine for the future.

 ?? ?? Below: Scanning Electronic Microscopi­c images of lateral view and internal view for ostracod specimens A1& 2) Loxoconcha zhejiangen­sis: right valve ( RV), juvenile; B1& 2) Neocypride­is sp.: left valve ( LV), adult; C1& 2) Neocythere­tta faceta: RV, adult; D1& 2) Neomonocer­atina delicata: LV, adult. Scale bar = 100 μm. Image credit: Yuanyuan Hong and Moriaki Yasuhara.
Below: Scanning Electronic Microscopi­c images of lateral view and internal view for ostracod specimens A1& 2) Loxoconcha zhejiangen­sis: right valve ( RV), juvenile; B1& 2) Neocypride­is sp.: left valve ( LV), adult; C1& 2) Neocythere­tta faceta: RV, adult; D1& 2) Neomonocer­atina delicata: LV, adult. Scale bar = 100 μm. Image credit: Yuanyuan Hong and Moriaki Yasuhara.
 ?? ?? Above: Infographi­c “Shells of benthic critters as a time machine into past and future marine ecosystems.” Credit: Created by NatureVolv­e.
Above: Infographi­c “Shells of benthic critters as a time machine into past and future marine ecosystems.” Credit: Created by NatureVolv­e.

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