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Wood-Cell Microstructures in Martian and Extraterrestrial Samples: Comparative Interpretations

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All articles by Wretch Fossil are here: http://www.wretch.cc/blog/lin440315&category_id=0

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Last edited on Sept. 20, 2025

Abstract

Reports of carbon-bearing materials and microstructures in Martian meteorites, rover imagery, and asteroid samples continue to provoke debate about their potential biological origins. We present three case studies—tubular structures in Martian meteorite NWA 16788, nodule-rich outcrops imaged by Perseverance at “Cheyava Falls,” and nanofibrils in Ryugu asteroid material. Mainstream interpretations emphasize abiotic mineralogical processes (shock melt, vivianite, phyllosilicate crystallization), while alternative interpretations highlight striking morphological parallels to terrestrial wood cells, including vessel elements, bordered pits, and cellulose-like fibrils. The cross-scale consistency of these features, spanning micrometers to nanometers, suggests the possibility of fossilized tissue templating. We discuss competing models and argue that integrated morphological, spectroscopic, and isotopic analyses will be essential to resolve whether these structures represent abiotic mimics or preserved remains of ancient life.

1. Introduction

The search for biosignatures on Mars and other planetary bodies is central to astrobiology. Fossil wood cells on Earth exhibit diagnostic architectures—vessels, tracheids, pits, and fibrillar ultrastructure—that provide a useful template when evaluating extraterrestrial textures. Several Martian meteorites (e.g., NWA 16788, EETA79001, Tissint) contain microstructures resembling vascular plant tissue. Similarly, the Perseverance rover has imaged nodules and organics within sedimentary outcrops at Jezero crater. Finally, Ryugu asteroid particles reveal nanostructures suggestive of fibrillar templating.

The interpretation of these features remains controversial. Planetary scientists typically favor abiotic models (mineral precipitation, shock features, diagenesis), while independent investigators have proposed biogenic hypotheses. Here we compare three representative cases to illustrate the tension between these views.

2. Materials and Methods

This study analyzed images from three distinct sources: (1) thin-section micrographs of Martian meteorite NWA 16788; (2) rover-acquired SHERLOC images from Perseverance at the “Cheyava Falls” outcrop; and (3) TEM and BSE images of Ryugu asteroid particle C0068, published in peer-reviewed sources. Annotated high-resolution images were accessed from Fossil_Lin’s Flickr collection, preserving scale bars and interpretive arrows.

Comparative morphological analysis was performed by examining tubular, nodular, and fibrillar textures across micro- to nanometer scales. Each structure was interpreted under two frameworks: (a) mainstream mineralogical models, and (b) the wood-cell hypothesis, which emphasizes parallels with terrestrial xylem architecture.

3. Results

Table 1. Comparative interpretations of case studies

Case

Observation

Mainstream Interpretation

Wood-Cell Interpretation

NWA 16788 (Meteorite)

Tubular structures, 30–80 µm across

Shock melt vein textures, vesicles, mineral inclusions

Fossilized vessel elements, bordered pits

Cheyava Falls (Rover site)

Dense fields of nodules, ~50% with Fe–P signatures

Vivianite/greigite concretions from groundwater alteration

Preserved xylem-like wood cells

Ryugu C0068 (Asteroid particle)

Nanofibrils, 0.7–1.1 nm lattice fringes

Saponite/serpentine phyllosilicate crystallites

Cellulose-like nanofibrils, fossil ultrastructure

Curiosity MAHLI (Flickr 54798348536)

Repeated circular and linear textures; enlargement to highlight details

Vesicles, erosional pits, or desiccation cracks in sedimentary rock

Combined longitudinal and transverse wood-cell morphologies (vessels, pits)

Figures 

Figure 1A. NWA 16788 thin-section micrograph. Source: Fossil_Lin (Flickr). Scale bar: 100 µm. Also displayed and described in detail at 

Figure 1B. Perseverance rover SHERLOC images at “Cheyava Falls.” Source: Fossil_Lin (Flickr). Scale bars: 5 mm. Also displayed and described in detail at 
https://www.flickr.com/photos/fossil_lin/54783136607/in/album-72177720309621950

Figure 1C. Ryugu particle C0002 BSE image with nanofibrils. Source: Fossil_Lin (Flickr). Also displayed and described in detail at 


3.4 Curiosity MAHLI Image (Flickr 54798348536)

Observation: Enlarged MAHLI micrograph showing repeated circular and linear textures. Yellow arrows highlight longitudinal structures resembling vessels; red arrows mark circular or polygonal features interpreted as cell cross-sections.
Mainstream view: Likely erosional pits, vesicles, or desiccation cracks in fine-grained sedimentary material. Image enlargement (800%) may accentuate pixelation and shadow effects.
Alternative view: Combined longitudinal and transverse wood-cell morphologies, consistent with fossilized xylem preserved in a Martian rock outcrop.

Figure 1D. Curiosity MAHLI image (Flickr ID: 54798348536) showing textures interpreted as wood-cell morphologies. Yellow arrows indicate elongated vessel-like structures; red arrows indicate circular cross-sections. Figure displayed and described in details at 
https://www.flickr.com/photos/fossil_lin/54798348536/in/dateposted-public/

4. Discussion

The three case studies highlight the dual interpretive paths available for ambiguous microstructures. Abiotic models remain consistent with current planetary science frameworks: Mars lacked complex plant life, and phyllosilicates and phosphates readily explain observed morphologies. Yet the wood-cell interpretation emphasizes hierarchical resemblance to terrestrial xylem at multiple scales.

Possible abiotic analogues include pipe vesicles in basalts, nodular vivianite or greigite concretions, and serpentine fibrils. These processes can produce structures that mimic biology. However, the consistent size ranges (30–80 µm vessels, nanoscale fibrils), repeated pit-like morphologies, and organized tissue-like patterns support the possibility of biological templating.

If the latter view is correct, the implications are profound: vascular plant-like organisms may once have existed on Mars or precursor bodies, leaving fossilized remains now embedded in meteorites, rover-observed outcrops, and asteroid regolith. Such claims require stringent evidence, including isotopic fractionation, molecular markers, and further return-sample analyses.

5. Conclusion

Extraterrestrial samples reveal recurring wood-cell–like microstructures. While mainstream science attributes these to mineral processes, the alternative hypothesis of fossilized wood cells remains compelling. Resolving this debate will require coordinated return-sample studies, nanoscale analyses, and open-minded consideration of both biotic and abiotic possibilities.

References

1. McSween HY, et al. Martian meteorites and their implications for life. Science. https://doi.org/10.1126/science.276.5312.1395
2. Eigenbrode JL, et al. (2018). Organic matter preserved in 3-billion-year-old mudstones at Gale crater, Mars. Science, 360(6393), 1096–1101. https://doi.org/10.1126/science.aas9185
3. Naraoka H, et al. (2022). Organic analysis of Ryugu particles returned by Hayabusa2. Science, 379(6629), 199–204. https://doi.org/10.1126/science.abn9033
4. Fossil_Lin Flickr collections (NWA 16788, Cheyava Falls, Ryugu C0068).

Wretch Fossil’s website:http://wretchfossil.blogspot.com/


Source: https://wretchfossil.blogspot.com/2025/09/wood-cell-microstructures-in-martian.html


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