- Scientists use several proxies to encapsulate the Earth's ancient climate. Pollen, diatoms, geochemical isotopes and fossils, for example, all contribute to linking past-climate puzzles together.
The ubiquity and wide geographic range of a variety of insects (eg nonbiting miz (Order Diptera, Family Chironomidae)), has recently made it a useful tool to recreate the Palaeolites around the world during the geological past.
Previous research used chironomids to reconstruct the climate during the Holocene (over the last 11,000 years), comparing fossil insects to modern intermediaries.
"This technique is] very good, but it has one major drawback: the farther back you go in time, the less applicable we know about coverage of modern animals becomes," a fossil from Ludwig Maximilian-University Says scientist Viktor Baranov. In Munich.
For example, the small dragonflies of today probably would not have shared a similar category with the meter-long dragonflies of the Cretaceous 100 million years ago, they point out.
Now, Baranov and his team have developed a technique to reach back in time, using the shape of the fossilized mizzle body and wings to recreate the temperature at the beginning of the Cretaceous, about 145 million years ago.
Barnov says that they wanted to add a proxy that could be useful for fossils found in geological settings where others might be unusable behind the scenes.
Their results, presented at the European Geoscience Union (EGU) General Assembly 2021, suggest that the relation of insect body size to latitude appears to be a promising new pseudo-palliative for paleotempers.
The possibility of using insects for deep paleoelastic work in the geologic past was fascinating, and Barnov says that he began to look at literature to see if it could be possible. Baranov says, "I notice that some workers have written in anecdotes written in very old papers — it appears that the Afrotropical representatives of this genus living in the Congo seem to be much younger than close relatives of France."
Considering the Bergman's rule that animals such as polar bears or Amur tigers living in the Arctic are considered large-sized animals, while their cousins in the tropics are small, Barnov thought that a body size could be Equally reliable, quantitative relationships may occur. And temperature "of fossil medians. To test his theory, he needed to begin measuring insects.
Measuring multiple mids
The ubiquity of insects makes them a good candidate for revealing global patterns, says Baranov. "In collections in Munich there are about 2 million specimens of chironomids from Antarctica to the Arctic, from Australia to England."
The team looked at 6,300 specimens that lived among the Tricic some time ago (245 million years ago) and today give good geographical location information. They measured the length of the body and wings, which showed that chironomids, both in the northern hemisphere, grew northward over their range. This means that, like polar bears, MiGs grew larger with colder temperatures.
Baranov says, "The average mood increases by one millimeter per five-degree latitude." "It was very exciting for me to learn. Because it means it's a very strong signal, at least in this group."
Baranov states that the results show the ability to use invertebrate fossils for quantitative analysis to reconstruct the Paleolithic period over millions of years.
Additionally, this temperature – size relationship can be useful in predicting what might happen to modern insect populations facing climate change. "I'm also working on the drivers of pest degradation and modern pest extinction," Barnov says. "It appears that rising temperatures affect the size of the insect, and it is affecting their ability to fly."