Initial Discoveries from the Rhizoliths Petrified Forest of Chania

This study presents the initial scientific characterization of the recently discovered Rhizoliths Petrified Forest of Chania, located at Stavros in the Akrotiri peninsula of Crete, Greece. Unlike most known petrified forests that primarily preserve tree trunks, this site uniquely features an abundan...

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Main Author: Emmanouil Manoutsoglou
Format: Article
Language:English
Published: MDPI AG 2025-06-01
Series:Heritage
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Online Access:https://www.mdpi.com/2571-9408/8/7/242
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author Emmanouil Manoutsoglou
author_facet Emmanouil Manoutsoglou
author_sort Emmanouil Manoutsoglou
collection DOAJ
description This study presents the initial scientific characterization of the recently discovered Rhizoliths Petrified Forest of Chania, located at Stavros in the Akrotiri peninsula of Crete, Greece. Unlike most known petrified forests that primarily preserve tree trunks, this site uniquely features an abundance of rhizoliths—fossilized root systems preserved through calcium carbonate mineralization. The rhizoliths exist within aeolianite formations along the coastal front, with diverse morphologies and sizes ranging from small trace-like forms to massive, branched structures exceeding one meter in length. The rhizoliths are exposed within historic Venetian quarries that operated from Minoan times through the medieval period at Stavros Bay, where quarrying operations have revealed these fossilized root systems preserved in coastal dune deposits. The site also contains in situ petrified trunks, calcrete formations, and biokarstic dissolution features that further enhance its scientific value. Microscopic examination of rhizolith samples has revealed valuable information about their internal structure, showing clear biogenic characteristics. The preservation of rhizolith structures and associated sedimentary features provides valuable insight into the Quaternary paleoenvironment, including former vegetation patterns, soil stabilization processes, and paleoclimatic conditions. The alternating layers of aeolianites and paleosols suggest cyclical environmental changes, with periods of active dune formation alternating with more stable conditions allowing soil development and vegetation establishment. This study documents the Stavros rhizoliths and their paleoenvironmental significance, contributing to the comparative understanding of similar features documented at other global sites.
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spelling doaj-art-d7577ff1c579477d8b4fdf715b17ae0f2025-08-20T02:45:52ZengMDPI AGHeritage2571-94082025-06-018724210.3390/heritage8070242Initial Discoveries from the Rhizoliths Petrified Forest of ChaniaEmmanouil Manoutsoglou0School of Mineral Resources Engineering, Technical University of Crete, 73100 Chania, GreeceThis study presents the initial scientific characterization of the recently discovered Rhizoliths Petrified Forest of Chania, located at Stavros in the Akrotiri peninsula of Crete, Greece. Unlike most known petrified forests that primarily preserve tree trunks, this site uniquely features an abundance of rhizoliths—fossilized root systems preserved through calcium carbonate mineralization. The rhizoliths exist within aeolianite formations along the coastal front, with diverse morphologies and sizes ranging from small trace-like forms to massive, branched structures exceeding one meter in length. The rhizoliths are exposed within historic Venetian quarries that operated from Minoan times through the medieval period at Stavros Bay, where quarrying operations have revealed these fossilized root systems preserved in coastal dune deposits. The site also contains in situ petrified trunks, calcrete formations, and biokarstic dissolution features that further enhance its scientific value. Microscopic examination of rhizolith samples has revealed valuable information about their internal structure, showing clear biogenic characteristics. The preservation of rhizolith structures and associated sedimentary features provides valuable insight into the Quaternary paleoenvironment, including former vegetation patterns, soil stabilization processes, and paleoclimatic conditions. The alternating layers of aeolianites and paleosols suggest cyclical environmental changes, with periods of active dune formation alternating with more stable conditions allowing soil development and vegetation establishment. This study documents the Stavros rhizoliths and their paleoenvironmental significance, contributing to the comparative understanding of similar features documented at other global sites.https://www.mdpi.com/2571-9408/8/7/242aeolianitefossilized root systemsfossilized trunksstumps and tree branchesdissolution pipescalcrete
spellingShingle Emmanouil Manoutsoglou
Initial Discoveries from the Rhizoliths Petrified Forest of Chania
Heritage
aeolianite
fossilized root systems
fossilized trunks
stumps and tree branches
dissolution pipes
calcrete
title Initial Discoveries from the Rhizoliths Petrified Forest of Chania
title_full Initial Discoveries from the Rhizoliths Petrified Forest of Chania
title_fullStr Initial Discoveries from the Rhizoliths Petrified Forest of Chania
title_full_unstemmed Initial Discoveries from the Rhizoliths Petrified Forest of Chania
title_short Initial Discoveries from the Rhizoliths Petrified Forest of Chania
title_sort initial discoveries from the rhizoliths petrified forest of chania
topic aeolianite
fossilized root systems
fossilized trunks
stumps and tree branches
dissolution pipes
calcrete
url https://www.mdpi.com/2571-9408/8/7/242
work_keys_str_mv AT emmanouilmanoutsoglou initialdiscoveriesfromtherhizolithspetrifiedforestofchania