Rhizobial root nodules in aeolian sandstones on Madeira (Piedade Beds, Pleistocene) and their significance for palaeonvironmental and "originator" hypotheses

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F44555601%3A13520%2F22%3A43897002" target="_blank" >RIV/44555601:13520/22:43897002 - isvavai.cz</a>

Výsledek na webu

<a href="https://www.sciencedirect.com/science/article/pii/S0034666722001385" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0034666722001385</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.revpalbo.2022.104740" target="_blank" >10.1016/j.revpalbo.2022.104740</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Rhizobial root nodules in aeolian sandstones on Madeira (Piedade Beds, Pleistocene) and their significance for palaeonvironmental and "originator" hypotheses

Popis výsledku v původním jazyce

Numerous rhizoliths were observed in aeolian Pleistocene sediments (ca. 80 ka) on the Ponta da Sao Lourenço Peninsula on easternMadeira. Surface of some rhizoliths locally exhibit bulbous swellings which were identified as rhizobial root nodules. Based on palaeoenvironmental analysis and a comparison with other rhizoliths in the Macaronesian region, the arborescent species of Morella faya, domestic to theMadeira Island, is suggested as the source taxon for the rhizoliths. Actinorhizal fungi of the genus Frankia are considered to be responsible for creating the nodules. Tree rhizoliths also document the changes in climate and plant cover composition on Madeira. Their origin dates to a rather humid period dominated by partly continuous arborescent vegetation.

Název v anglickém jazyce

Rhizobial root nodules in aeolian sandstones on Madeira (Piedade Beds, Pleistocene) and their significance for palaeonvironmental and "originator" hypotheses

Popis výsledku anglicky

Numerous rhizoliths were observed in aeolian Pleistocene sediments (ca. 80 ka) on the Ponta da Sao Lourenço Peninsula on easternMadeira. Surface of some rhizoliths locally exhibit bulbous swellings which were identified as rhizobial root nodules. Based on palaeoenvironmental analysis and a comparison with other rhizoliths in the Macaronesian region, the arborescent species of Morella faya, domestic to theMadeira Island, is suggested as the source taxon for the rhizoliths. Actinorhizal fungi of the genus Frankia are considered to be responsible for creating the nodules. Tree rhizoliths also document the changes in climate and plant cover composition on Madeira. Their origin dates to a rather humid period dominated by partly continuous arborescent vegetation.

Druh

J_ost - Ostatní články v recenzovaných periodicích

CEP obor

—

OECD FORD obor

10506 - Paleontology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2022

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Review of Palaeobotany and Palynology

ISSN

0034-6667

e-ISSN

0034-6667

Svazek periodika

306

Číslo periodika v rámci svazku

104740

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

8

Strana od-do

1-8

Kód UT WoS článku

—

EID výsledku v databázi Scopus

2-s2.0-85137099072