the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.
the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.
Drowning in a sandy ocean: Epiarenic growth of Tillandsia in the hyperarid Atacama Desert
Abstract. The Atacama Desert hosts a unique ecosystem formed by the sand-dwelling Tillandsia landbeckii, which extends over hundreds of square kilometers. This vegetation relies primarily on fog as its main water source; however, aeolian sand also plays a crucial role in the long-term persistence of both the species and the overall plant community. The terrain is sloped and exposed to the prevailing wind direction. Tillandsia forms regular banding patterns oriented orthogonally to these landscape features. In this study, we aim to elucidate the abiotic–biotic interactions between sand properties and vegetation characteristics through a comparative approach. Three populations – Caldera, Oyarbide and Arica –, each spanning several square kilometers in the southern, central, and northern regions of the Chilean Atacama Desert, were selected to compare wind regimes, terrain structure, sand and substrate properties, and vegetation structure in order to identify common principles that maintain vegetation integrity. Data were collected from six climate stations, 1,246 substrate samples, population genomic data from 718 individuals, as well as satellite imagery and digital terrain models. Our findings demonstrate that regional wind systems transport sand from distant source areas, while near the ground, Tillandsia vegetation reduces wind velocity and traps sand, leading to the formation of moderately sorted sandy substrates that are similar across all three populations. Sites lacking or containing dead Tillandsia individuals often differ significantly in substrate characteristics. Genetic analyses indicate that Tillandsia populations exhibit strong spatial structure albeit recruiting high genetic diversity and an excess of heterozygosity, reflecting adaptation to the dynamic environmental conditions. We conclude that sand represents an essential component of this ecosystem, while Tillandsia, as the dominant biotic factor, actively shapes and maintains this distinctive desert environment.
Status: open (until 03 Jul 2026)
- RC1: 'Comment on egusphere-2026-1429', Nicholas Lancaster, 22 May 2026 reply
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CC1: 'Comment on egusphere-2026-1429', Xiaoping Yang, 29 May 2026
reply
The paper combing geomorphology, sedimentology, climatology and plant DNA offers an interesting perspective for experts in different fields, and particularly for those studying desert ecosystem both in Atacama and globally. The study shows that there is a correlation between grain size features, fog frequency and growth of plants in the Atacama. I am impressed by the efforts of collecting various kind of data including climate, DSM, sediments and plant DNA in such a remote area from Heidelberg.
I believe the paper could be better if the authors would consider some level of revisions. Also I think the section of Conclusions is too short. More details should be added to this section. I think the introduction section should be more focused. In its current version the introduction contains some of the general knowledge and it is not needed for a research paper. About five pages for introduction are indeed too long for my taste.
As the annual precipitation is extremely low in the study areas, it is needed to indicate the duration of the observations for calculating the mean annul precipitation in Fig. 1 and in the text.
As a geomorphologist I do not know much about methods of DNA. I believe the methodologies of sedimentology are fine. Even though I would like to ask about the meaning of sorting. See Lines 365-370: I think sorting degree cannot be directly measured with an absolute range due to general variations of grain size. Within coarse sands 1.27 um is a little but quite a lot if it is clay type of sediments.
Citation: https://doi.org/10.5194/egusphere-2026-1429-CC1
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This is an interesting manuscript that combines geomorphology and DNA-based population genetics to understand monospecific populations of Tillandsia in the hyper arid Atacama Desert and their relations to sand transport by wind.
The manuscript is very long and reads like a report to sponsors. It could benefit from severe pruning to make it more concise and to tell the authors' story more effectively.. At the same time, it does lack information on the physical and biotic character of the investigated sites. Numerous correlations between variables are discussed but no plots are included.
Introduction – very long and introduces multiple topics – monospecific plant communities, dryland ecosystems, banded vegetation patterns, Tillandsia communities. We finally learn the objectives of this paper at line 220.
Theis section needs to focus on Tillandsia ecosystems in the Atacama and their distinctive characteristics and not ecological theory. Some subheadings would be helpful
Methods
Very detailed documentation of sample collection and analysis.
Results
This section could benefit from some reorganization of material in order to present first the physical environment and then the biotic information. This section could benefit from some site photographs to show the environments in which the Tillandsia grow
785 – it is aspect, not exposition here and in this section
Discussion
This section is very generalized and discusses broader aspects of Tillandia ecology especially in relation to climate change. It does not easily follow from the result presented here. Some more detailed discussion of relationships between topography, winds, sand transport and particle size should be included here
Conclusions
do not follow from the results of the field and laboratory studies documented here