Three Ways Ashore: Where Did Terrestrial Plants, Arthropods and Vertebrates Come from? Are Essentiality Patterns of Chemical Elements Living Bio(-Geo)chemical "Fossils"? - Inferences from Essentiality Patterns and the Biological System of Elements

• Autorzy: Franzle S. , Markert B.

Warianty tytułu

PL

Trzy drogi na ląd: skąd wywodzą się rośliny lądowe, stawonogi i kręgowce? Czy bio(-geo)chemiczne "skamieliny" odwzorowują rozkład istotnych pierwiastków chemicznych żywych organizmów? - wnioski wyciągnięte z rozkładu pierwiastków istotnych oraz...

• Języki publikacji: EN

Abstrakty

EN

Among other topics the Biological System of Elements [3] comprehensively describes the distribution of chemical elements in glycophyte plants, regardless whether these elements are essential, (presumably) non-essential or outright toxic. This approach has also been applied to other taxa, phyla and even kingdoms. However, comparisons among different kingdoms of organisms which separated about one billion years ago (fungi, algae, higher plants, animals) show large differences among the sets of essential elements. Thus evolutionary changes render it impossible to reconstruct the whereabouts of the ancestors of groups of recent organisms (geochemical palaeoecology) from comparisons of element essentialities Ys. the relative abundances of these and other elements in sea- and fresh water, respectively. Losses of ions from the tissues of fresh-water fishes are controlled by the extent of complexation. The selection pressure to go ashore was larger in fresh water. Probably the number of essential elements was larger soon after evolution of metazoans, adaptation to live with fewer ones being most pronounced in fungi.

PL

Wśród innych obecnie rozpatrywanych podejść, Biologiczny System Pierwiastków Chemicznych (BSE) zrozumiale opisuje podział pierwiastków chemicznych w roślinach glikofitowych, bez względu na to, czy te pierwiastki są istotne, (przypuszczalnie) nieistotne lub też ewidentnie toksyczne. Takie podejście zastosowano również do innych grup taksonomicznych i gromad, a nawet królestw. Jednak porównania różnych królestw organizmów, które rozdzieliły się ok. l miliarda lat temu (grzyby, algi, rośliny wyższe, zwierzęta), pokazują duże różnice między zestawieniami pierwiastków istotnych. A zatem zmiany ewolucyjne sprawiają, że nie jest możliwa rekonstrukcja miejsca przebywania przodków współczesnych grup organizmów (paleontologia geochemiczna) poprzez porównanie względnego rozpowszechnienia w nich pierwiastków istotnych oraz innych pierwiastków z takimi danymi dla wody słodkiej i morskiej. Ubytki jonów z tkanek ryb słodkowodnych są kontrolowane przez zakres ich skompleksowania. Napór do wyjścia na ląd był większy dla organizmów słodkowodnych. Prawdopodobnie liczba pierwiastków istotnych była większa krótko po pojawieniu się tkankowców. Adaptacja do życia z mniejszą liczbą tych pierwiastków jest najbardziej wyraźna u grzybów.

Słowa kluczowe

EN

biological system of elements evolution; metalloproteins; essentiality; food chains; optimal catalytic ions

PL

biologiczny system pierwiastków chemicznych; ewolucja; metaloproteiny; istotność; łańcuchy pokarmowe; optymalne katalityczne jony

• Wydawca: Towarzystwo Chemii i Inżynierii Ekologicznej
• Czasopismo: Chemia i Inżynieria Ekologiczna
• Rocznik: 2002
• Tom: Vol. 9, nr 9
• Strony: 949--967
• Opis fizyczny: Bibliogr. 50 poz., rys., tab.

Twórcy

autor

Franzle S.

• International Graduate School (IHI) Zittau, Markt 23, D-02763 Zittau, Germany

autor

Markert B.

• International Graduate School (IHI) Zittau, Markt 23, D-02763 Zittau, Germany

Bibliografia

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