Cavolinia inflexa is a species of small pteropod.
| Cavolinia inflexa | |
|---|---|
Scientific classification  | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Mollusca |
| Class: | Gastropoda |
| Clade: | Euopisthobranchia |
| Order: | Pteropoda |
| Family: | Cavoliniidae |
| Genus: | Cavolinia |
| Species: | C. inflexa |
| Binomial name | |
| Cavolinia inflexa (Lesueur, 1813) | |
Cavolinia inflexa are members of the thecosome pteropod genus that dwell in the epipelagic zone feeding on arctic snow and smaller microorganisms. While it is known that Cavolinia inflexa are filters feeders, their reproductive tendencies and behaviors are not well studied. They can be used as a proxy for assuming climatic conditions for a particular period and have been a focus of ocean acidification impact studies. [1] [2]
Like other thecosome pteropods, Cavolinia inflexa form an aggronite shell to surround their body. As a result, they have been found to be highly sensitive to ocean acidification and the constantly changing water column’s chemical composition. [3] Cavolinia inflexa are found to be between 2-8 millimeters in length, and have a length to width ratio between 0.51 and 0.81. Additionally, they have a straight shell, their posterior tip bent upwards, and a bilaterally symmetrical structure. [4]
Cavolinia inflexa move throughout depths in response to where the largest concentration of food is, as it reacts to the vertical migration patterns expressed by zooplankton. [5] However, they are mostly found floating in the epipelagic zone of the ocean. Their vertical migration is also in response to a diurnal cycle. [6] They feed by ingesting their captured prey that has been snared by their mucus feedings webs. After 1-3 minutes they can completely consume and digest their snared prey. [7]
Information on the reproduction of Cavolinia inflexa is scant, but there has been research conducted on the reproduction of similar pteropod species. The pteropod Limacina retroversa has a reproductive cycle occurring twice a year. [8] The first occurring at the start of spring and the second nearing the end of summer. In order to survive and reproduce, the two distinct generations employ different life history strategies. Offspring born during the spring reproductive cycle develop more rapidly so they can mature in time for the summer mating season while offspring born during the summer withstand the physiological challenges of the cold winter to then reproduce the following spring. [8] It takes at least 3 months of development for Limacina retroversa to produce viable egg clutches. [9]
Cavolinia inflexa are a common thecosome pteropod found worldwide in warm waters between 55° N to 45° S. [3] They are filter feeders as is typical among Pteropoda. Their diet consists of marine snow–organic matter that is suspended in the water column.
Cavolinia inflexa were initially believed to be multiple subspecies, but later studies show that the species does not exhibit enough regional variation to have categorical subspecies. [4] Cavolinia inflexa live in the Atlantic, Indian, and Pacific Oceans, but there is not significant geographical variation. [4]
Climate change may pose a threat to Cavolinia inflexa as ocean acidification has been shown to impact larval development. [2] In particular, ocean acidification prevents the formation of their shells, leaving the organism vulnerable to predation. [3] One study found a significant decrease in shell density among Cavolinia inflexa between 1910 and 2012. [10]
The Thecosomata, or sea butterflies, are a taxonomic suborder of small, pelagic, free-swimming sea snails known as holoplanktonic opisthobranch gastropod mollusks, in the order Pteropoda. Most pteropods have some form of calcified shell, although it is often very light, even translucent.
Sea angels are a large group of small free-swimming sea slugs, not to be confused with Cnidarians, classified into six different families. They are pelagic opisthobranchs in the clade Gymnosomata within the larger mollusc clade Heterobranchia. Sea angels were previously referred to as a type of pteropod.
The mesopelagiczone, also known as the middle pelagic or twilight zone, is the part of the pelagic zone that lies between the photic epipelagic and the aphotic bathypelagic zones. It is defined by light, and begins at the depth where only 1% of incident light reaches and ends where there is no light; the depths of this zone are between approximately 200 to 1,000 meters below the ocean surface.
Limacina is a genus of swimming predatory sea snails commonly known as sea butterflies in the family Limacinidae. This genus contains some of the world's most abundant gastropod species.
The Notobranchaeidae, or "naked sea butterflies", are a taxonomic family of floating sea slugs, specifically under the subclass Opistobranchia, also called "sea angels".
Pteropoda are specialized free-swimming pelagic sea snails and sea slugs, marine opisthobranch gastropods. Most live in the top 10 m of the ocean and are less than 1 cm long. The monophyly of Pteropoda is the subject of a lengthy debate; they have even been considered as paraphyletic with respect to cephalopods. Current consensus, guided by molecular studies, leans towards interpreting the group as monophyletic.
Pelagic fish live in the pelagic zone of ocean or lake waters—being neither close to the bottom nor near the shore—in contrast with demersal fish that live on or near the bottom, and reef fish that are associated with coral reefs.
Argonauta bottgeri, also known as Böttger's argonaut, is a species of pelagic octopus belonging to the genus Argonauta. The female of the species, like all argonauts, creates a paper-thin eggcase that coils around the octopus much like the way a nautilus lives in its shell.
Diel vertical migration (DVM), also known as diurnal vertical migration, is a pattern of movement used by some organisms, such as copepods, living in the ocean and in lakes. The adjective "diel" comes from Latin: diēs, lit. 'day', and refers to a 24-hour period. The migration occurs when organisms move up to the uppermost layer of the water at night and return to the bottom of the daylight zone of the oceans or to the dense, bottom layer of lakes during the day. DVM is important to the functioning of deep-sea food webs and the biologically-driven sequestration of carbon.
Marine larval ecology is the study of the factors influencing dispersing larvae, which many marine invertebrates and fishes have. Marine animals with a larva typically release many larvae into the water column, where the larvae develop before metamorphosing into adults.
The deep scattering layer, sometimes referred to as the sound scattering layer, is a layer in the ocean consisting of a variety of marine animals. It was discovered through the use of sonar, as ships found a layer that scattered the sound and was thus sometimes mistaken for the seabed. For this reason it is sometimes called the false bottom or phantom bottom. It can be seen to rise and fall each day in keeping with diel vertical migration.
Clione limacina, known as the naked sea butterfly, sea angel, and common clione, is a sea angel found from the surface to greater than 500 m (1,600 ft) depth. It lives in the Arctic Ocean and cold regions of the North Atlantic Ocean. It was first described by Friderich Martens in 1676 and became the first gymnosomatous "pteropod" to be described.
Limacina helicina is a species of small swimming planktonic sea snail, in the family Limacinidae. It belongs to the group commonly known as sea butterflies (Thecosomata).
Limacina rangii is a species of swimming sea snail in the family Limacinidae, which belong to the group commonly known as sea butterflies (Thecosomata).
Limacina retroversa is a distinct species of swimming planktonic gastropods, belonging to a group of predatory sea snails known as sea butterflies (Thecosomata). The name Limacina retroversa describes the unique morphology of this sea snail, including its slug-like body and coiled, backwards-turning shell. They are typically found in the epipelagic zone of cold, polar waters, but can be found worldwide, in any ocean. L. retroversa are currently under threat, as their numbers are decreasing due to rising global carbon levels and other human-caused climate threats.
The Arctic Ocean covers an area of 14,056,000 square kilometers, and supports a diverse and important socioeconomic food web of organisms, despite its average water temperature being 32 degrees Fahrenheit. Over the last three decades, the Arctic Ocean has experienced drastic changes due to climate change. One of the changes is in the acidity levels of the ocean, which have been consistently increasing at twice the rate of the Pacific and Atlantic oceans. Arctic Ocean acidification is a result of feedback from climate system mechanisms, and is having negative impacts on Arctic Ocean ecosystems and the organisms that live within them.
Human activities affect marine life and marine habitats through overfishing, habitat loss, the introduction of invasive species, ocean pollution, ocean acidification and ocean warming. These impact marine ecosystems and food webs and may result in consequences as yet unrecognised for the biodiversity and continuation of marine life forms.
Elizabeth M. Harper (Liz) is an evolutionary biologist known for her work on molluscs. She is an honorary fellow of the British Antarctic Survey and was accorded the title of Honorary Professor by the University of Cambridge in 2019.
Diacria trispinosa is a holoplanktonic species of gastropods belonging to the family Cavoliniidae. It is classified as a mesoplankton. It is a pteropod.
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