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Anthropocene Extinctions
May 9, 2022
Tikalon is located in a widely
forested suburban area of
Northern New Jersey, and
woodland animals are often sighted on our
streets. These are mostly
deer, but several years ago a large
brown bear nearly destroyed our
high-density polyethylene (HDPE) garbage can at
curbside as it was looking for
food. The increased
sprawl of
humanity across the
Earth has affected
animal behavior and
survivability in several ways.
Not only is there a loss of animal
habitat, but there's also
habitat fragmentation caused by
roadways that prevent free animal movement. These same roadways are responsible for
air,
noise, and
light pollution that lead to diminished animal
health and increased
mortality. A decade ago, a deer crossing a highway collided with my
wife's car as she was driving one
morning. The deer was apparently not
injured, but
damage to the car was extensive.
A mother deer and her fawns.
This photograph was taken early in the morning on July 16, 2021, when the animals were foraging on the lawn across from my house.
(Photo by the author. Click for larger image.)
Our present
geological epoch is the
Holocene, a name constructed from the
Greek word ʿολος (holos, "entirely") combined with a
suffix, -cene, indicating something recent; so, we live in a period that's "entirely recent." The Holocene is defined as starting 11,700 years before the year 2000, and this was the start of the
Neolithic Era (New Stone Age) of
human development, at which time there were
globally only about five million people.
Things got slightly crowded by the
first century, when there were more than a hundred million people, increasing to a billion by
1800. From that point, humanity has grown more than a thousand fold to our
present population of more than 7 billion, and such a large number is enough to significantly change their
environment.
Humanity has wrought so much change on Earth that
geologists are defining a new
Anthropocene geological epoch in the
geologic time scale, with a name derived from the Greek word for human, ἄνθρωπος (anthropos). Since these are geologists, they are attempting to define an easily located
stratigraphic marker of human presence, a "
golden spike." They have appeared to settle on evidence of humans from the
mid-twentieth century, the start of the
Great Acceleration, a time of very rapid
socioeconomic expansion and the
Atomic Age. I wrote about the Anthropocene in two previous articles,
The Anthropocene, January 18, 2016, and
Anthropocene Minerals, August 16, 2021.
Any geological marker of the Anthropocene should be easily discovered, and modern
technology has produced many geological
artifacts. In a span of less than an
average human lifetime, humans have consumed more
energy than in the twelve
millennia since the start of the Neolithic. Modern-day
strata contain abundant
plastics,
concrete and
supermarket chicken bones. Other Anthropocene markers are
deforestation,
animal husbandry,
carbon dioxide (CO2),
methane (CH4),
plant and animal extinction, and a spike in the diversity and distribution of
mineral-like compounds.[1-3]
Two
botanists from the
Smithsonian National Museum of Natural History,
John Kress, Senior Research Botanist and
Emeritus Curator of Botany, and
Gary A. Krupnick of the
Plant Conservation Unit, have recently
published an
open access paper in the
journal,
Plants, People, Planet that examines human impact on plant
species biodiversity.[4-5] They've found that plant species are going
extinct because people don't need them.[4-5]
While species may tolerate slight shifts in their habitat conditions and
adapt, or
migrate to new habitats, those that can't may become extinct.[4] Humans have found some plant species to be useful and have therefore
domesticated them, but others have been driven to extinction.[4] A related concept is
co-evolution that drives
unnatural selection in which creatures
symbiotic with us have greatly prospered; for example,
cattle,
rice, and the
eucalypts.[4]
In their study, the Smithsonian researchers classified about 30% of
vascular plant species, such as
lycophytes,
ferns,
gymnosperms, and
angiosperms, as being either
winners or
losers in the Anthropocene.[4] They found that losers greatly outnumber winners, and that this trend will continue in the future.[4] The researchers also mapped the winners and losers, both
taxonomically and
phylogenetically, across the major groups of vascular plants.[4] They classified 86,592 species into seven categories, as follow:[4]
• Winners useful to humans.
• Winners not useful to humans.
• Losers useful to humans.
• Losers not useful to humans.
• Tentative winners.
• Potential losers.
• Currently neutral species.
Plant winners and losers in the Anthropocene. (a) Ginkgo biloba, (b) Prunus serotina, (c) Magnolia ekmanii, (d) Ceratozamia kuesteriana, (e) Halophila stipulacea, (f) Merremia tuberosa, (g) Araucaria muelleri, (h) Sidalcea stipularis, (i) Cirsium canescens, (j) Asclepias oenotheroides, (k) Grusonia pulchella, (l) Cleisostoma porrigens, (m) Cytisus oromediterraneus, (n) Carex bullata, (o) Cyanea comata, and (p) Eryngium sarcophyllum. (Fig. 1 of ref. 4, licensed under a Creative Commons License (See figure caption in reference for additional details).[4] Click for larger image.)
The results show many more loser species than winners; and, if present trends continue, future losers will continue to greatly outnumber future winners.[4] Although winners and losers are distributed through nearly all the
orders of vascular plants, all but two of the nine major phylogenetic
lineages favor losers over winners.[4] Some of the smaller
ancestral orders might be at risk of extinction.[4-5] There are 6,749 winner plants; and these, such as
corn, rice,
wheat, are those helpful to humans.[5] There is also the
curious case of plants now extinct in the wild, such as the
ginkgo tree, but survive in cities.[5]
Ginkgo biloba is a
popular ornamental tree also used for food, and as a
dietary supplement.[5] There are 164 winners which are not useful to humans, such as the
invasive kudzu.[5]
Among the 20,290 loser species are the
Haitian magnolia tree, cut for
firewood,
redwoods and
junipers, and the ancient
conifer,
Araucariaceae.[5] 26,002 species are potential losers, 18,664 species are potential winners, and 571 plant species have already become extinct.[5] The trend is towards less biodiversity, and this will lead to a loss of animal diversity and more vulnerable
ecosystems.[5] Plant
communities will be much more
homogenized in the future.[5] The existence of
seed banks and
cryogenic tissue storage means that any plant can be saved from extinction, but an effort must be made to do even such small
mitigation.
Ginkgo biloba are large trees of size ranging from 20-50 meters.
Ginkgo biloba is the last living species in the order Ginkgoales, and the genus Ginkgo was found in the Middle Jurassic about 170 million years ago.
Extracts of Ginkgo biloba leaf are sold as a cognitive enhancer, but there is no evidence that it promotes enhanced memory or attention in healthy people.
(Wikimedia Commons image by Piott.)
References:
- Griffin Chure, Rachel A. Banks, Avi I. Flamholz, Nicholas S. Sarai, Mason Kamb, Ignacio Lopez-Gomez, Yinon M. Bar-On, Ron Milo, and Rob Phillips, "The Anthropocene by the Numbers: A Quantitative Snapshot of Humanity's Influence on the Planet," arXiv, January 24, 2021.
- Robert M. Hazen, Edward S. Grew, Marcus J. Origlieri, and Robert T. Downs, "On the mineralogy of the 'Anthropocene Epoch'," American Mineralogist: Journal of Earth and Planetary Materials, vol. 102, no. 3 (March, 2017), pp. 595-611.
- Catalog of 208 human-caused minerals bolsters argument to declare 'Anthropocene Epoch', Carnegie Science and the Deep Carbon Observatory Press Release, March 1, 2017.
- W. John Kress and Gary A. Krupnick, "Lords of the biosphere: Plant winners and losers in the Anthropocene," Plants, People, Planet, March 10, 2022, https://doi.org/10.1002/ppp3.10252.
- Sofia Quaglia, "Plants humans don't need are heading for extinction, study finds," The Guardian, March 10, 2022.
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