Exploring the limitations of asteroid crater lakes as climate archives

Drill core from borehole taken in 1981 from the Nördlinger Ries. There are distinctive layers of light-colored dolomite between fine-layered dark sediments of the former crater lake. Credit: Gernot Arp, Göttingen University In southern Germany just north of the Danube, there lies a large circular depression between the hilly surroundings: the Nördlinger Ries. Almost 15

Liked this post? Share with others!

Hexbyte Glen Cove

Drill core from borehole taken in 1981 from the Nördlinger Ries. There are distinctive layers of light-colored dolomite between fine-layered dark sediments of the former crater lake. Credit: Gernot Arp, Göttingen University

In southern Germany just north of the Danube, there lies a large circular depression between the hilly surroundings: the Nördlinger Ries. Almost 15 million years ago, an asteroid struck this spot. Today, the impact crater is one of the most useful analogs for asteroid craters on early Mars.

Studying the deposits of the former lake that formed in the crater is particularly informative. These deposits have been of great interest ever since NASA began exploring Martian craters for signs of water and life on Mars. However, the chemical development of the former and its habitable areas is only partially understood.

An international research team led by the University of Göttingen has now uncovered clues about the past: they analyzed dolomite rocks in a drill core and found an extremely high proportion of the carbon isotope C-13. Further investigations traced this back to a phase of strong methane formation by microorganisms known as archaea in water with a low sulfate content.

In contrast, the sediments of the previous, first phase of the crater lake showed clear traces of high sulfate content and bacterial sulfate decomposition. This change reveals that the groundwater pathways to the lake changed as the cooled. The results have been published in the journal Geochimica et Cosmochimica Acta.

A 250-meter-long drill core taken in 1981 provided information about the during the time periods that sediment was being deposited in the crater lake. Combining sedimentological, biogeochemical and isotope geochemical research methods enabled the researchers to identify a distinctive section, which they investigated in more detail using biomarker analyses.

Scanning electron microscope image using material taken in the drill core from the borehole taken in 1981 from the Nördlinger Ries reveals dolomite crystals with rhombohedral shape. Credit: Lingqi Zeng, Göttingen University

They detected organic biomarkers originating from sulfate-reducing bacteria and “normal” dolomite in older rocks from the crater lake. In the younger rocks, they found dolomite enriched with C-13 and a chemical called archaeol which indicates that archaea were present at that time.

The properties of the rocks reflect the conditions in the crater lake during their formation: the decrease in sulfate is due to degradation by bacteria and the C-13 enrichment is due to the formation of methane by archaea.

“This chemical development can only be explained by the change in the groundwater supply during the gradual cooling of the crater floor. This led to a change from deep, hydrothermal groundwater (with sulfate) to cooler water without sulfate that must have flowed through limestone rocks near to the surface,” explains study leader Professor Gernot Arp from the Department of Geobiology at the University of Göttingen.

The findings not only provide important information on the development of the crater lake being investigated, but also, as Arp notes, “Our findings show that the conditions in asteroid crater lakes are strongly controlled by internal processes such as crater floor cooling and water supply. In contrast, are of secondary importance, unlike in many other lakes. This must be taken into account when deposits in terrestrial and extraterrestrial craters are used as climate archives to deduce past climate conditions from the sediments.”

More information:
Lingqi Zeng et al, Extremely 13C-enriched dolomite records interval of strong methanogenesis following a sulfate decline in the Miocene Ries impact crater lake, Geochimica et Cosmochimica Acta (2023). DOI: 10.1016/j.gca.2023.10.013

Citation:
Exploring the limitations of asteroid crater lakes as climate archives (2023, December 5)
retrieved 6 December 2023
from https://phys.org/news/2023-12-exploring-limitations-asteroid-crater-lakes.html

This document is subject to copyright. Apart from any fair dealing for the purpose of private study or research, no
part may be reproduced without the written permission. The content is provided for information purposes only.

% %item_read_more_button%% Hexbyte Glen Cove Educational Blog Repost With Backlinks — #metaverse #vr #ar #wordpress

Subscribe to our newsletter

Collect visitor’s submissions and store it directly in your Elementor account, or integrate your favorite marketing & CRM tools.

Do you want to boost your business today?

This is your chance to invite visitors to contact you. Tell them you’ll be happy to answer all their questions as soon as possible.

Learn how we helped 100 top brands gain success