Gaiman Formation

Gaiman Formation
Stratigraphic range: Burdigalian (Colhuehuapian)
~19.8–17.5 Ma

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Gaiman Formation; Stratigraphic range: Burdigalian (Colhuehuapian); ~19.8–17.5 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓
Type	Geological formation
Underlies	Puerto Madryn Formation
Overlies	Sarmiento Formation
Thickness	70 m (230 ft)
Lithology
Primary	Mudstone, sandstone
Other	Tuff, phosphate
Location
Coordinates	43.3°S 65.3°W
Approximate paleocoordinates	44.0°S 59.2°W
Region	Chubut Province
Country	Argentina
Extent	Peninsula Valdés Basin
Type section
Named for	Gaiman
Named by	Mendía & Bayarsky
Year defined	1981
	Gaiman Formation (Argentina)

The Gaiman Formation (Spanish: Formación Gaiman), in older literature also referred to as Patagonian Marine Formation (Spanish: Formación Patagonia Marino, Patagoniense), is a fossiliferous geologic formation of the Peninsula Valdés Basin in the eastern Chubut Province of northwestern Patagonia, eastern Argentina.

The 70 metres (230 ft) thick formation overlies the Sarmiento Formation and is overlain by the Puerto Madryn Formation and comprises grey and white tuffaceous mudstones and sandstones, deposited in a shallow marine environment.

The Gaiman Formation has provided fossils of many extinct penguins, among which five species in the genus Palaeospheniscus, as well as whales and dolphins, most notably Aondelphis talen, Prosqualodon australis, Idiorophus patagonicus and Argyrocetus patagonicus, indeterminate seal and turtle fossils, shark and other fossils. The richness of the formation, and the other formations in the area, such as the underlying Sarmiento Formation, led to the establishment of the Bryn Gwyn Paleontological Park, with a Welsh name, reflecting the amount of Welsh settlers in the region.

Description

Outcrop map and stratigraphic column of the Gaiman Formation in the Peninsula Valdes Basin

The Gaiman Formation was first defined by Mendía & Bayarsky in 1981,[1] and further described by Mendía in 1983, taking its name from Gaiman in Chubut Province, eastern Patagonia.[2] Gaiman in the local language of the native Tehuelche people means "rocky point".[3] The formation crops out in the lower course of the Chubut River,[4] and overlies the continental Trelew Member of the Sarmiento Formation and is overlain by the Late Miocene Puerto Madryn Formation. The formation is 70 metres (230 ft) thick,[5] and comprises marine tuffs, tuffaceous mudstones, sandstones and coquinas.[1]

The Gaiman Formation is correlated with the Chenque Formation of the Golfo San Jorge Basin and the Monte León Formation of the Austral Basin to the south, the Saladar Member of the lower Gran Bajo del Gualicho Formation of the Colorado Basin to the north and the Vaca Mahuida Formation of the Neuquén Basin to the northwest.[6]

Depositional environment

Middle Miocene (15 Ma)

The basal stratum of the Gaiman Formation is a thin transgressive lag with some gravels, bones and teeth from marine vertebrates.[5] The unit displays a concentration of phosphatic concretions, ooids, bones and teeth.[7] The marine sediments overlying this basal stratum are composed of white, tuffaceous, thoroughly bioturbated mudstones and fine sandstones with occasional mollusk molds and thin oyster horizons, deposited in a shallow shelf environment.[5]

The marine transgression leading to the deposition of the Gaiman Formation is the first of two major South Atlantic transgressions of the Miocene, the second causing the deposition of the overlying Puerto Madryn Formation.[8]

Facies analysis shows that the formation represents a transgressive-regressive stratigraphic cycle, with palaeoenvironments including coastal, storm-dominated shoreface, inner shelf embayment and open inner shelf.[9]

The age of the Gaiman Formation is established on stratigraphic correlations to other absolutely-dated sections in Patagonia and biostratigraphic data and dates to the Early Miocene (Burdigalian, or Colhuehuapian in the SALMA classification).[5]

Paleontological significance

Fossils of the Gaiman Formation in the Bryn Gwyn Paleontological Park

The Gaiman Formation has provided several fossil penguins, of which nine are assigned to specific species and include five species of the genus Palaeospheniscus. Also, shark teeth, fossils of indeterminate seals and turtles, and several dolphins, baleen and toothed whales have been found in the formation. Argentine paleontologist Florentino Ameghino described an isolated tooth from the formation first as an ichthyodectiform fish, Portheus patagonicus in 1901, however this fossil was assigned to a delphinoid cetacean of the family Kentriodontidae by Cione and Cozzuol in 1990.[10] Fish recorded from the formation are hexanchiform hexanchids, lamniform isurids, odontaspidids, cetorhinids, carcharhiniform carcharhinids, heterodontiform heterodontids, squatiniform squatinids myliobatiform myliobatids, perciform oplegnathids and labrids, and tetraodontiform molids.[11] Rays are abundant in the formation.[12] The lack of somatic remains of most molluscs, bryozoans, polychaetes and cirripeds in the formation is attributed to the high-energy and corrosive environment at time of deposition, as well as diagenesis after the formation was deposited.[13]

The bird species Eretiscus tonnii solely occurs in the Gaiman Formation.[14] Bite marks on several of the penguin bones are attributed to terrestrial mammals such as didelphid or hathliacyniid sparassodont marsupials, common in Patagonia during the Miocene.[15] Other ichnofossils found on the bones are presumably caused by dental erosion by regular echinoids,[16] and bite marks by sharks, as Galeocerdo aduncus.[17]

The paleontological richness of the formation, as well as the more fossiliferous underlying Sarmiento Formation, led to the establishment of the Bryn Gwyn Paleontological Park.[18]

Fossil content

The formation has provided the following fossils:[19][20][21][22][23]

Class	Group	Fossils	Notes
Mammals	Dolphins	Aondelphis talen	[24]
		Dolgopolis kinchikafiforo	[25]
		Kentriodon sp.	[12]
		Eurhinodelphinidae indet.	[20]
	Toothed whales	Argyrocetus patagonicus	[12]
		Idiorophus patagonicus	[26]
		Phoberodon arctirostris	[12]
		Prosqualodon australis	[12][27]
		Squalodontidae indet.	[20]
	Baleen whales	Aglaocetus moreni	[26]
		Morenocetus parvus	[26]
		Plesiocetus dyticus	[26]
	Seals	Phocidae indet.	[22]
Birds	Penguins	Apterodytes ictus	[21]
		Eretiscus tonnii	[28]
		Palaeospheniscus bergi syn Palaeospheniscus planus, P. rothi	[28][19]
		Palaeospheniscus bilocular	[28]
		Palaeospheniscus gracilis	[20]
		Palaeospheniscus patagonicus syn Palaeospheniscus affinis, P. intermedius, P. interruptus	[19][29]
		Palaeospheniscus wimani	[22]
		Paraptenodytes antarcticus	[28]
		Paraptenodytes robustus syn. Treleudytes crassa	[19][29]
		Arthrodytes sp.	[20]
		Sphenisciformes indet.	[20]
	Anseriformes	Cayaoa bruneti	[4][30]
	Anseriformes	Anseriformes indet.	[20]
Reptiles	Turtles	Dermochelyidae indet.	[20]
Fish	Sharks	Carcharoides totuserratus	[17]
		Echinorhinus pozzii	[12]
		Galeocerdo aduncus	[17]
		Megascyliorhinus trelewensis	[12]
		Heterodontus sp.	[12]
		Odontaspis sp.	[12]
		Pristiophorus sp.	[12]
		Squalus sp.	[12]
	Oplegnathidae	Oplegnathus sp.	[12]
Mollusks	Bivalves	Crassostrea ?hatcheri	[23]
	Bivalves	Balanus sp.	[31]
	Gastropods	Turritella sp.	[31]
Ichnofossils	Bioturbation	Chondrites, Ophiomorpha, Planolites, Skolithos	[11]
	Bite marks	Gnathichnus pentax	[16]
	Bite marks	Entobia	[16]