PALAEOLOVE’s Time and Group Code

008September 1, 2015

If we are interested in wildlife or the evolution of animals and plants, respectively their behaviour, ecological requirements or systematics, we will encounter disciplines of organismic biology (neontology) and palaeobiology (palaeontology). The same will happen if we are interested, e.g., in mushrooms/fungi or early and primitive life.

Organismic disciplines are amongst others zoology/botany, physical anthropology/palaeoanthro­pology (natural history of man and other primates) or palaeozoology/palaeobotany.

The neontological disciplines (zoology, physical anthropology, botany) scientifically cultivate the fields of recent or living organisms, the palaeontological ones (palaeozoology, palaeoanthropology, palaeobotany) carry out investigations on former life or fossil (=/≠ prehistoric) taxa. Organismic research on living specimens is conducted by direct observations or profound analyses of body functions (physiology) etc. Scientific interpretations of fossils are based on comparative anatomy, functional morphology and so on as well as on the biology of related or ecologically similarly adapted living organisms and the application of their biology to the extinct taxa under study. Thus, the mode of life or palaeobiology of fossils can be interpreted and it is possible to prepare life reconstructions to visualise them for the public.

As a rule the animals and plants presented on this website lived as a rule after the Cambrian explosion or radiation in the course of the last 541 million years of Earth history or are existing today – but some may be older. The Cambrian explosion was a relatively short evolutionary event during which most major animal groups appeared. Since then life on Earth has well been documented by the fossil record due to «nature’s invention of biomineralization» (the capability of organisms to produce hard tissues).

The mushrooms/fungi presented here are recent organisms; offered examples of early and primitive live can be both, recent or fossil.

PALAEOLOVE’s Time and Group Code

The task of the PALAEOLOVE’s Time and Group Code is to directly inform visitors and customers of their favoured organism groups via our homepage and to guide them to the appropriate objects, artwork or illustrated items.

For Animals and Plants the following non-black Time Code is used
= recent, living in the present
= recently extinct (subfossil), vanished during the Holocene* (the last 11700 years)
= fossil, existed before the Holocene*

For Mushrooms/Fungi and Early & Primitive Live the following black Time Code is used
= recent, living in the present
= fossil, existed before the Holocene*

visible on product pages and the page Picture & Object Info, a menu item of the main menu and the middle footer menu.

The current Geologic Time Scale / Chronostratigraphic Chart with a fine subdivision of Earth’s history (relative time sequences) and up-to-date numerical ages (absolute time data) published by the International Commission on Stratigraphy can be looked up > here

The Group Code for directly accessible Popular Organismic Groups of Interest

This code is used together with a product code for the Product Categories showing up on the shop page and to some extent also for the Publication Categories (see below) on the blog side bar:

  • Fossil Organisms
  • Fossil Vertebrates/Craniota (also used as Publication Category in the blog)
  • Non-Avian Dinosaurs
  • Fossil Invertebrates (also used as Publication Category in the blog)
  • Recent Organisms
  • Recent Vertebrates/Craniota (also used as Publication Category in the blog)
  • Recent Invertebrates (also used as Publication Category in the blog)
  • Marine Reptiles
  • Marine Mammals
  • Active & Passive Flight

Another possibility to find your preferred organisms and associated items quickly is the use of our menu item Systematic Product Index in the main menu and the middle footer menu.


* The Holocene is part of the Quaternary. The current subdivision of the latter is: Pleistocene, Holocene. It is discussed to complement the Quaternary with a third geologic epoch called the Anthropocene to separate and cover the most recent part of Earth history when human activities started to have a significant global impact on the ecosystems of our planet. Currently the eligibility of the proposed new epoch is evaluated and a suitable start discussed.

© 2024 Palaeolove. Science meets Design — Website by SteckDesign