Spore

In biology, a spore is a unit of sexual (in fungi) or asexual reproduction that may be adapted for dispersal and for survival, often for extended periods of time, in unfavourable conditions.

The main difference between spores and seeds as dispersal units is that spores are unicellular, the first cell of a gametophyte, while seeds contain within them a developing embryo (the multicellular sporophyte of the next generation), produced by the fusion of the male gamete of the pollen tube with the female gamete formed by the megagametophyte within the ovule.

Below is a table listing the mode of classification, name, identifying characteristic, examples, and images of different spore species.

Some markings represent apertures, places where the tough outer coat of the spore can be penetrated when germination occurs.

[9] Envelope-enclosed spore tetrads are taken as the earliest evidence of plant life on land,[10] dating from the mid-Ordovician (early Llanvirn, ~470 million years ago), a period from which no macrofossils have yet been recovered.

[11] Individual trilete spores resembling those of modern cryptogamic plants first appeared in the fossil record at the end of the Ordovician period.

[12] In fungi, both asexual and sexual spores or sporangiospores of many fungal species are actively dispersed by forcible ejection from their reproductive structures.

Attracting insects, such as flies, to fruiting structures, by virtue of their having lively colours and a putrid odour, for dispersal of fungal spores is yet another strategy, most prominently used by the stinkhorns.

In Common Smoothcap moss (Atrichum undulatum), the vibration of sporophyte has been shown to be an important mechanism for spore release.

[15] In the case of spore-shedding vascular plants such as ferns, wind distribution of very light spores provides great capacity for dispersal.

[18] The spores found in microfossils, also known as cryptospores, are well preserved due to the fixed material they are in as well as how abundant and widespread they were during their respective time periods.

[3] Both cryptospores and modern spores have diverse morphology that indicate possible environmental conditions of earlier periods of Earth and evolutionary relationships of plant species.

Spores produced in a sporic life cycle.
Fresh snow partially covers rough-stalked feather-moss ( Brachythecium rutabulum ) , growing on a thinned hybrid black poplar ( Populus x canadensis ) . The last stage of the moss lifecycle is shown, where the sporophytes are visible before dispersion of their spores: the calyptra ( 1 ) is still attached to the capsule ( 3 ). The tops of the gametophytes ( 2 ) can be discerned as well. Inset shows the surrounding, black poplars growing on sandy loam on the bank of a kolk , with the detail area marked.
Sporangium of Fungi
Zygospores on Rhizopus
Ascospores of Didymella Rabiei
Typical reproductive structure of a basidiomycete , including the basidiospore and basidium
Aecia on foliage
Uredinospores
Microscopic image of teliospores
Light microscopy of Polysiphonia showing a carpospores and carposporophyte inside
Tetraspores of Polysiphonia
A parasitic pink fungi on a Lichen tree
In plants , microspores , and in some cases megaspores, are formed from all four products of meiosis.
In contrast, in many seed plants and heterosporous ferns , only a single product of meiosis will become a megaspore (macrospore), with the rest degenerating.
Ascomycete containing mitospores
Microscopic image of a Zoospore
Autospores of a strain of Jenufa aeroterrestrica
Ballistospore mechanism of dispersal from fungi
Puff Balls containing Stratismospores
Fossil trilete spores (blue) and a spore tetrad (green) of Late Silurian origin
Tricolpate pollen of Ricinus
Spores being ejected by fungi.