Cavolinia inflexa

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Introduction

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]

Contents

Morphology and Physiology

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]

Behavior

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]

Life Cycle and Reproduction

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]

Ecology and Distribution

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]

Cavolinia inflexa
Naturalis Biodiversity Center - RMNH.MOL.233660 - Cavolinia inflexa (Lesueur, 1813) - Cavoliniidae - Mollusc shell.jpeg
Scientific classification Red Pencil Icon.png
Kingdom: Animalia
Phylum: Mollusca
Class: Gastropoda
Subclass: Heterobranchia
Order: Pteropoda
Family: Cavoliniidae
Genus: Cavolinia
Species:
C. inflexa
Binomial name
Cavolinia inflexa
(Lesueur, 1813)

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<i>Limacina</i> Genus of gastropods

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<span class="mw-page-title-main">Cavolinioidea</span> Superfamily of gastropods

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The Notobranchaeidae, or "naked sea butterflies", are a taxonomic family of floating sea slugs, specifically under the subclass Opistobranchia, also called "sea angels".

<i>Paedoclione doliiformis</i> Species of gastropod

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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.

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<span class="mw-page-title-main">Cavoliniidae</span> Family of gastropods

The family Cavoliniidae is a taxonomic group of small floating sea snails, pelagic marine opisthobranch gastropod mollusks.

<i>Clione limacina</i> Species of gastropod

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.

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Limacina helicina is a species of small swimming planktonic sea snail in the family Limacinidae, which belong to the group commonly known as sea butterflies (Thecosomata).

<i>Limacina rangii</i> Species of gastropod

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.

<span class="mw-page-title-main">Ocean acidification in the Arctic Ocean</span>

The Arctic ocean covers an area of 14,056,000 squared 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.

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<i>Diacria trispinosa</i> Species of gastropod

Diacria trispinosa is a holoplanktonic species of gastropods belonging to the family Cavoliniidae. It is classified as a mesoplankton.

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References

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  3. 1 2 3 Doney, Scott C.; Fabry, Victoria J.; Feely, Richard A.; Kleypas, Joan A. (2009-01-01). "Ocean Acidification: The Other CO 2 Problem". Annual Review of Marine Science. 1 (1): 169–192. doi:10.1146/annurev.marine.010908.163834. ISSN   1941-1405.
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  5. Tarling, G. A., Matthews, J. B. L., David, P., Guerin, O., & Buchholz, F. (2001). The swarm dynamics of northern krill (Meganyctiphanes norvegica) and pteropods (Cavolinia inflexa) during vertical migration in the Ligurian Sea observed by an acoustic Doppler current profiler. Deep Sea Research Part I: Oceanographic Research Papers, 48(7), 1671-1686.
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  8. 1 2 Dadon, J.R., de Cidre, L.L. (1992). The reproductive cycle of the Thecosomatous pteropod Limacina retroversa in the western South Atlantic. Marine Biology 114, 439–442.
  9. Thabet, A.A., Maas, A.E., Lawson, G.L. et al. (2015). Life cycle and early development of the thecosomatous pteropod Limacina retroversa in the Gulf of Maine, including the effect of elevated CO2 levels. Mar Biol162, 2235–2249.
  10. Howes, E.L., Eagle, R.A., Gatusso, J.P. (2017). Comparison of Mediterranean pteropod shell biometrics and ultrastructure from historical (1910 and 1921) and present day (2012) samples provides baseline for monitoring effects of global change. PLOS One.

[1] [2] [3] [4] [5] [6] [7] [8] [9] [10] [11]


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  4. Doney, S.C., Fabry, V.J., Feely, R.A., Kleypas, J.A. (2009). Ocean acidification: the other CO2 problem. Annual Review of Marine Science, 1, 169-192.
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