Sea mink

The sea mink (Neogale macrodon) is a recently extinct species of mink that lived on the eastern coast of North America around the Gulf of Maine on the New England seaboard. It was most closely related to the American mink (Neogale vison), with continuing debate about whether or not the sea mink should be considered a subspecies of the American mink (as Neogale vison macrodon) or a species of its own. The main justification for a separate species designation is the size difference between the two minks, but other distinctions have been made, such as its redder fur. The only known remains are bone fragments unearthed in Native American shell middens. Its actual size is speculative, based largely on tooth remains.

The sea mink was first described in 1903, after its extinction; information regarding its external appearance and habits stem from speculation and from accounts made by fur traders and Native Americans. It may have exhibited behavior similar to the American mink, in that it probably maintained home ranges, was polygynandrous, and had a similar diet, though more seaward-oriented. It was probably found on the New England coast and the Maritime Provinces, though its range may have stretched further south during the last glacial period. Conversely, its range may have been restricted solely to the New England coast, specifically the Gulf of Maine, or just to the nearby islands. The largest of the minks, the sea mink was more desirable to fur traders and became extinct in the late 19th or early 20th century.

The sea mink was first described as Lutreola macrodon, distinct from the American mink, by Daniel Webster Prentiss, a medical doctor and ornithologist, in 1903, after it became extinct. Prentiss based his description on skull fragments recovered from Native American shell middens in New England. Most sea mink remains, nearly all of them skull fragments, have come from shell middens, but a complete specimen has never been found.

Debate has occurred regarding whether the sea mink was its own species, or another subspecies of the American mink. Those who argue that the sea mink was a subspecies often refer to it as Neovison vison macrodon. A study in 1911 by Frederic Brewster Loomis, an American paleontologist, concluded that the differences between the American mink and the sea mink were too minute to justify the latter's classification as a separate species, and he named it Lutreola vison antiquus. A study conducted in 2000 by Mead et al. refuted Loomis by claiming that the size range for the largest sea mink specimen was beyond that of the American mink, thereby making it a separate species. But a 2001 study by Graham concluded that this size difference was insufficient evidence to classify the sea mink as its own species and that it should be considered a subspecies. Graham supposed that the size difference was caused by environmental factors. Furthermore, Graham reported that Mead assumed the smaller mink specimens to be the American mink, and the larger mink specimens outside the range of the American mink to be sea minks; this may have been a case of sexual dimorphism wherein all specimens were sea minks, the larger ones being males and the smaller ones being females. A 2007 study compared the dental makeup of the sea mink to the American mink, and concluded that they were distinct enough to be considered two separate species.

The taxonomy of the minks was revised in 2000, resulting in the formation of a new genus, Neovison, which includes only the sea mink and the American mink. Formerly, both minks were classified in the genus Mustela. The species name macrodon translates to "large teeth". According to Richard Manville, a naturalist who maintains that the sea mink is not a separate species, its closest relative is the common mink (N. v. mink), which also inhabits the New England area. A 2021 study into New World weasels found that the sea mink, along with four other extant species, should be classified into a new genus, Neogale.

Fur traders who hunted it gave the sea mink various names, including water marten, red otter, and fisher cat. Possibly the first description of this species was made by Sir Humphrey Gilbert in the late 1500s as "a fish like a greyhound", which was a reference to its affinity for the sea and its body shape and gait, which were apparently similar to that of a greyhound. It is possible that the fisher (Pekania pennanti) got its name from being mistakenly identified as the sea mink, which was also known as the fisher by fur traders. The Abenaki Indians referred to it as the "mousebeysoo", which means "wet thing". It was named "sea mink" because it was always found near the coast by fur traders, and subsequently the American mink was often referred to as the "woods mink".

The sea mink was a marine mammal that lived around the rocky coasts of New England and the southernmost Maritime Provinces until it was hunted to extinction in the late 19th or early 20th century. Most sea mink remains are unearthed on the coast of Maine. Though it is speculated that they at one point inhabited Connecticut and Rhode Island, they were commonly trapped along the coast of the Bay of Fundy (in the Gulf of Maine), and it is said that they formerly existed on the southwestern coast of Nova Scotia. There were reports of unusually large mink furs being collected from Nova Scotia regularly. The bones of a specimen unearthed in Middleboro, Massachusetts, were dated to be around 4,300±300 years old, 19 kilometers (12 mi) from salt water. The sea mink may have reached that area by traveling up rivers, or may have been brought there by Native Americans. The latter is most likely, as no other mink remains have been discovered between Casco Bay in Maine and southeastern Massachusetts. Sea mink bones have been unearthed in Canada, although these may have been carried there by Native Americans from the Gulf of Maine. The rugged shorelines of the Down East region of Maine may have represented a northernmost barrier in their range. Mead concluded that only American minks inhabited the mainland and that sea minks were restricted to islands off the coast. If this is the case, then all remains found on the mainland were carried there. Graham challenged that hypothesis, stating that it is unlikely that all sea mink specimens originate from one population.

During the last glacial period, ending 12,000 years ago, the sea mink's range may have extended south of the Gulf of Maine. It may have even evolved there, as Maine at that time would have been covered in glaciers, although the oldest known specimen only dates back to around 5,000 years; this could be due to the rising sea levels—older sea mink remains may be submerged underwater. Alternately, the sea mink may have evolved after the last glacial period and filled a new ecological niche.