Year by Year
Explore Year by Year articles from the most modern historical year back to the oldest.
3,307 Articles Archived
Cork Predators
Archived: 15 September 2026
31,622 BCE is not a datable Irish historical event but an imprecise modern label within Marine Isotope Stage 3. Derryvree, County Fermanagh, records organic freshwater sediments between glacial advances, indicating locally ice-free, treeless wetlands with mosses, sedges and pools. Greenagho and Crag Cave likewise demonstrate fluctuating climates rather than continuous ice cover. Castlepook Cave, County Cork, preserves reindeer, mammoth, horse and carnivore remains, evidencing an open, cold landscape supporting large mammals. A marked reindeer femur may indicate stone-tool butchery by humans about 33,000 BCE, but lacks secure context. Subsequent ice expansion probably erased or buried landscapes and traces of visits.
Sedge Pools
Archived: 15 September 2026
31,623 BCE is a label within a resolved Late Pleistocene interval, not an Irish year. Derryvree, County Fermanagh, preserves freshwater sediments between glacial tills, dated to encompass this horizon, indicating ice-free, periglacial tundra wetlands with pools, mosses, sedges and insects. Ireland was approaching, rather than experiencing, the Last Glacial Maximum. Castlepook Cave in north Cork contains cold-stage fauna, including mammoth, reindeer and predators, though deposits are mixed. A marked reindeer femur may indicate human carcass processing, but cannot prove settlement. Together, these sparse archives show fluctuating habitats, faunal connectivity and possible human presence, while excluding precise chronology or social narratives.
Glacial Intervals
Archived: 15 September 2026
Approximately 31,624 BCE, Ireland lay within the unstable Marine Isotope Stage 3 cold period, not a precisely identifiable historical year. Inter-till deposits at Derryvree, Greenagho and Hollymount in Fermanagh show episodes of ice-free freshwater tundra later overridden by glaciers. Plant and insect remains indicate open, treeless, periglacial environments, while fluctuating sea levels and ice complicated access to the island. Castlepook Cave in County Cork preserves bones of mammoth, reindeer, giant deer, bears, wolves and hyaenas, reflecting intermittent cold-adapted fauna. A possibly cut-marked reindeer bone suggests, but does not prove, Upper Palaeolithic human activity. No institutions or political history are known.
Arctic Foxes
Archived: 15 September 2026
31,625 BCE is a modern label for an uncertain interval within Marine Isotope Stage 3, not a recoverable Irish year. Derryvree, County Fermanagh, preserves freshwater sediments between glacial tills, dated broadly to 36,900–31,700 cal BP, indicating cold, open periglacial wetlands with sedges and mosses. Castlepook Cave, County Cork, contains fauna including reindeer, mammoth, hyaena and Arctic fox, demonstrating intermittent links with wider European ecosystems. A marked reindeer femur may indicate human butchery around 33,000 years ago, but cannot prove settlement. Evidence supports changing climates, temporary animal access and possible brief human visits, while society, culture and permanent occupation remain unknown.
Elusive Toolmark
Archived: 15 September 2026
31,626 BCE is a modern label within Marine Isotope Stage 3, not a recorded Irish year. Evidence from Derryvree indicates cold freshwater, tundra and steppe-tundra habitats between glacial episodes, while Ireland probably comprised open ground, meltwater, frozen terrain and advancing ice. Castlepook Cave preserves a long, mixed animal record including mammoth, reindeer, giant deer and predators. A reindeer femur, dated about 33,000 years ago, bears possible stone-tool cut marks, suggesting but not proving brief Upper Palaeolithic human activity. No secure settlement, tools, hearths, burials or cultural identity are known. Ireland's past is defined by change, fauna and uncertain human passage.
Juniper Marshland
Archived: 15 September 2026
At the modern date 31,627 BCE, Ireland lay in the climatically unstable later Pleistocene, approaching the Last Glacial Maximum. Evidence is sparse and disrupted by later ice. Buried organic beds at Derryvree, County Fermanagh, indicate an ice-free interval with treeless, cold muskeg of mosses, sedges, herbs, dwarf willow and juniper. Castlepook Cave, County Cork, preserves remains of mammoth, hyaena, reindeer, giant deer and other fauna, indicating varied open habitats and links with wider Europe. A cut-marked reindeer femur may record human carcass processing, but cannot prove permanent settlement. No political, cultural or social history is recoverable; environmental change dominates here.
Derryvree Peatland
Archived: 15 September 2026
Around 31,628 BCE, a modern and necessarily imprecise label, Ireland lay in the fluctuating late Pleistocene MIS 3 interval, before the Last Glacial Maximum. Derryvree, near Maguiresbridge, preserves organic silts between glacial tills, showing an ice-free freshwater mosaic of tundra-like, largely treeless vegetation, insects and wet peaty ground. Castlepook Cave in Cork contains a chronologically mixed assemblage including mammoth, reindeer, giant deer and predators, demonstrating intermittent cold-stage animal communities. A marked reindeer bone may indicate brief Upper Palaeolithic human activity, but remains contested. Evidence cannot establish permanent settlement, routes, social life or events; later ice severely obscured much earlier landscapes.
Fermanagh Basins
Archived: 15 September 2026
Around 31,629 BCE, Ireland lay in an early, uneven phase of last-glacial ice-sheet growth, with some regions retaining freshwater basins and open periglacial landscapes. Deposits at Derryvree and Greenagho show that parts of Fermanagh remained habitable for cold-adapted ecosystems before later glaciation. Castlepook Cave in County Cork yielded rich Late Pleistocene remains, including mammoth, giant deer, reindeer, bears and spotted hyenas. A roughly 33,000-year-old reindeer bone possibly bears stone-tool damage, suggesting a human visit, but no settlement evidence exists. Lower sea levels may have aided movement, though routes remain unknown. This period represents ecological richness, fragmentary evidence and advancing ice.
Periglacial Grasslands
Archived: 15 September 2026
Around 31,630 BCE, Ireland lay within an unstable Ice Age interstadial, before the Last Glacial Maximum but amid shifting ice margins, low seas and varied regional conditions. Cave remains at Castlepook, County Cork, document Late Pleistocene fauna including mammoth, reindeer, giant deer, bears, wolves and hyaenas, indicating episodic open, cold-steppe habitats, though not a single contemporaneous ecosystem. Buried sediments at Derryvree, County Fermanagh, reveal treeless periglacial wetlands with grasses, sedges, herbs and mosses. Human occupation remains unproven: a possibly cut-marked reindeer bone may suggest visitors, but lacks secure context. Later glaciation destroyed evidence, leaving changing environments rather than social history.
Doneraile Mammals
Archived: 15 September 2026
Around 31,631 BCE, Ireland lay in the unstable later Marine Isotope Stage 3, before the Last Glacial Maximum. Cold, open, largely treeless habitats supported reindeer, mammoth, giant deer, bears and hyaenas, although advancing ice and changing seas made access uncertain. Castlepook Cave near Doneraile preserves a long, disturbed faunal record. A reindeer femur, dated about 33,000 years ago, bears a possible stone-tool butchery mark, suggesting fleeting human activity but not settlement or continuous occupation. Derryvree sediments in Fermanagh record cold tundra wetland conditions between ice advances. Together, these fragmentary archives indicate active landscapes and possible human visitation before widespread glaciation.
Some records do not yet have a verified historical year and are awaiting chronological placement.